Content uploaded by Rachel Coppock
Author content
All content in this area was uploaded by Rachel Coppock on Nov 06, 2018
Content may be subject to copyright.
Microplasticsinmarinefoodwebs
OuSetälä
1
,MaijuLehniemi
1
,RachelCoppock
2,3
,MahewCole
2,3
1
MarineResearchCentre,FinnishEnvironmentInstute,P.O.Box140,00251Helsinki,Finland
2
MarineEcologyandBiodiversityGroup,PlymouthMarineLaboratory,PlymouthPL13DH,UnitedKingdom
3
CollegeofLifeandEnvironmentalScience:Biosciences,UniversityofExeter,ExeterEX44QP,UnitedKingdom
Microplastic debris is a globally‐pervasive contaminant, which presents a substantial risk to marine
biota, food webs and ecosystems. Microplastics are heterogeneously distributed, with highest
concentrations associated with the oligotrophic subtropical gyres, and relatively
biologically‐productive semi‐enclosed seas and coastal waters. Encounter rates between biota and
microplastics are driven by their geographical overlap and relative concentrations, as well as the
characteristics of the plastic, and the motility, detection capabilities and feeding strategy of the
organism. We identify four main routes via which microplastics can infiltrate marine food webs:
ingestion, inhalation, entanglement and trophic transfer. Drawing upon established research and
more recent exposure studies using microplastics, we highlight how plastics can be detected,
ingested, processed and rejected by filter feeders. Finally, we consider how marine organisms can
affect microplastics, by incorporating the plastic into biological matrices, through to the movement,
redistributionandburialofplastic.
Introduction
A multude of food webs exist in the world's oceans, made up of a wide variety of organisms
that occupy disnct niches and possess different behavioral and feeding strategies. So far, only a
small fracon of these taxa have been included in studies concerning microplasc debris in marine
ecosystems. Microplascs (microscopic plasc debris, 100 nm ‐ 5 mm diameter) are now widely
recognised as a pollutant of internaonal concern (Galgani et al., 2013; GESAMP 2016).
Understanding the potenal impacts this prolific contaminant can have on marine life and food webs
has become of intense interest, with an exponenal increase in research being conducted in recent
years. In this chapter we explore how microplascs enter marine food webs, and consider the
complex, iterave relaonship between microplascs, biota and biologically‐mediated ecological
processes. Microplasc ingeson has been documented in animals throughout the marine food web,
including zooplankton (Desforges et al., 2014), fish (Bellas et al., 2016; Lusher et al., 2013), marine
mammals (Lusher et al., 2015; Bravo‐Rebolledo et al., 2013), turtles (Nelms et al., 2015) and seabirds
(Tourinho et al., 2010). We explore the factors affecng microplasc consumpon and infiltraon
into marine food webs, with consideraon given to spaal overlap, predator‐plasc raos, the
properes of microplasc debris, and the life‐history and feeding‐strategies of biota demonstrated to
consume plasc. At the individual level, microplascs pose a risk to the health of the organism;
indeed, a growing number of experimental studies have demonstrated that at crical concentraons,
microplascs can adversely affect feeding, energec reserves, reproducon, growth and survival in
invertebrate and vertebrate species, including calanoid copepods (Cole et al., 2015; Lee et al., 2013),
polychaete worms (Wright et al., 2013; Green et al., 2016), fish (Rochman et al., 2015) and oysters
(Sussarellu et al., 2016). The latest evidence suggests that microplascs could also affect higher levels
of biological organisaon, with populaon shis and altered behaviour impacng upon the ecological
funcon of keystone species (Galloway et al., 2017). While the risks microplascs pose to individual
biota are explored in greater detail in other chapters of this book, here we focus on how plascs have
the potenal to affect food webs and marine ecosystems as a whole. Furthermore, we consider how
trophicinteraconsandecologicalprocessescanchangethemicroplascsthemselves.
INFOBOX1:Methodologicalapproach
Although microplascs are a relavely new topic in the environmental sciences, researchers
have been able to learn from the experimental approaches and understanding gleaned from the
fields of ecotoxicology, marine biology, and aquac chemistry. Basic mechanisms of feeding and
energy transfer in marine food webs are well understood, and this knowledge has been useful in
understanding observed interacons between microplascs and biota. Lessons learnt from
nanoparcle research have been of parcular relevance to microplascs exposure studies,
parcularly in respect to uptake mechanisms and mechanisms underpinning observed health effects,
as well as developing sound ecological risk assessment (Syberg et al., 2015; Hüffer et al., 2017). In
contrast, collecng field data on the distribuon and quanty of microplascs in different ecological
compartments (water surface, water column, seafloor habitats, strandline) has turned out to be a
significant challenge, requiring novel approaches, method development and opmisaon
(Hidalgo‐Ruz et al., 2012; Lusher et al., 2017). An ongoing issue facing microplascs researchers is the
absence of harmonised sampling or sample analyses protocols, and a forward challenge for the field
istoworktowardsmethodologicalstandardisaon.
Theoverlapbetweenplasticsandbiota
Perhaps the most important variable affecng the flux of microplasc parcles into marine food
websistheirabundanceanddistribuonintheenvironment,andphysicaloverlapwithbiota.
Geographicaloverlap
In recent years, there has been a concerted effort to idenfy the different habitats polluted
with plasc debris, and ascertain the concentraons of microplascs across a wide range of aquac
ecosystems. Microplascs are ubiquitous in the world´s oceans, and their presence in remote
locaons, including the Arcc (Lusher et al., 2015), Antarcc (Waller et al., 2017), mid‐oceanic atolls
(Do Sul et al., 2014) and the oceanic depths (Woodall et al., 2014), have highlighted their widespread
distribuon. However, accurately determining the concentraons and type of microplascs present
in seawater and sediments has proven a challenge. Adaptaons to tradional sampling techniques
(e.g. trawls, sediment grabs; see review by Hidalgo‐Ruz et al., 2012) have proven invaluable for
collecng samples, however isolang and idenfying microplascs has required a more novel
approach (see INFOBOX 1). In recent years, a wide range of methodologies have been suggested for
extracng and analysing plascs (see reviews by Lusher et al., 2017 and Miller et al., 2017), however
the variety of methods employed can oen result in incomparable datasets. Analysing such data is
further confounded by the heterogenous distribuon and temporal variability in microplasc
concentraons.
Global sampling efforts have helped to idenfy ‘hotspots’ of plasc (Eriksen et al., 2014, Cozar
et al., 2015, van Sebille et al., 2015). For example, the North Pacific, South Pacific and North Atlanc
subtropical oceanic gyres, which amass flotsam from throughout the oceanic basins, have all been
highlighted as accumulaon zones for microplasc debris (Moore et al., 2001; Law et al., 2010;
Eriksen et al., 2013). Oceanic gyres are largely oligotrophic and therefore relavely devoid of marine
life, however for biota that can survive in the gyres, interacons with microplasc will be
commonplace. For example, in the North Pacific gyre, Moore et al., (2001) observed a 6:1 plasc to
plankton rao, and Goldstein & Goodwin (2013) idenfied 33% of gooseneck barnacles (Lepas spp.)
had consumed between 1 and 30 items of microplasc. However, our understanding of the numbers
and distribuon paerns of microplascs in marine environments is far from complete. This was
pointed out already in the study dataset of >330 µm parcles from surface water tows, which
showed smallest parcles to be most prevalent, but only down to a certain size group (1 mm) aer
which the concentraons decreased (Cozar et al., 2014). This absence of smaller plasc may result
from difficules in idenfying very small parcles, or might be explained by bioc or abioc
degradaonormovementoftheseplascs.
Enclosed and semi‐enclosed seas like the Mediterranean Sea and the Balc Sea have also been
noted for their high microplasc concentraons (Collignon et al., 2914, Setälä et al., 2016b and
Gewert et al., 2017) and thus have been proposed to accumulate plasc debris in greater amounts
than open oceans (Fossi et al., 2016). As increasing concentraons inevitably increase the exposure
of organisms at the base of the food webs, this may be the case also at higher trophic levels. In the
Mediterranean Sea, stomach analyses from large pelagic predators (swordfish and tuna) revealed
that 18.5% of the fish examined contained microplascs. The reported concentraons of
microplascs from the surface waters of another highly polluted semi‐enclosed sea basin, the Balc
Sea, show how the microplasc concentraons in surface waters may significantly differ spaally
(Setälä et al., 2016b, Gewert et al., 2017), and may reach high concentraons (up to 4.7 x 105 km
‐2
)
close to highly populated urban areas with low water exchange, or as was found by Gorokhova
(2015), in deep water layers separated by a halocline. In the Balc Sea the field observaons of
microplascs in the food web have mainly related to fish, herring being the most studied fish species.
Bråte et al., (2017) analyzed the data from various studies on microplascs in fish from these Nordic
waters; in the analyzed dataset consisng of 1425 individuals of Atlanc and Balc herring,
microplasc ingeson varied between 0 and 30%. Ogonowski et al., (2017) reported that
approximately 50% of herring individuals had ingested plascs along the Swedish coast in the Balc
Sea, although the numbers of microplascs on individual fish were low (0‐1/fish), reflecng great
variability between samples. In comparison, very low numbers of parculate microplascs (fibres
were excluded) were also found in a recent study containing over 500 herring individuals from the
open sea areas of the northern Balc Sea (Budimir et al., in press). The reported share of herring
with ingested microplasc parcles varies greatly between these studies, and may at least partly be
explained by spaal differences in the overlap of microplascs and herring. Differences in methods
used for extracng microplascs from fish ssue makes comparisons between studies difficult and
conclusionsvague.
A recent study predicts the greatest overlap between microplascs and marine life will occur
in coastal regions (Clark et al., 2016). Coastal waters and estuaries have relavely high biological
producvity owing to their shallow, protected waters and fresh nutrional inputs from rivers, which
are valued by aquaculture and fisheries, and encompass important nursery grounds for
commercially‐exploited marine taxa. It is postulated that their proximity to sources of anthropogenic
polluon (e.g. marime industry, urban areas, riverine inputs), puts them at high risk of microplasc
polluon. Microplasc sampling in coastal regions is problemac owing to the density of organic
material in these waters (Cole et al., 2014), nevertheless recent studies have highlighted the overlap
between plascs and biota in coastal waters. In the English Channel, a 36.5% incidence of
microplasc ingeson in demersal and pelagic fish species has been observed (Lusher et al., 2013),
while 70% of brown shrimp (Crangon crangon) sampled from the coastlines of European countries
along the English Channel have been shown to consume microplasc (Devriese et al., 2015). More
recently, Steer et al., (2017) idenfied the rao of microplascs to fish larvae ranged from 1:27
nearestPlymouth(UnitedKingdom),to1:135kmfromtheshoreline.
Habitats
Microplascs consist of a wide range of polymers which have their own special characteriscs
that affect their distribuon in the water, and thereby which organisms and habitats are prone to
plasc exposure. Local wind condions, water currents as well as geomorphology all affect the
distribuon of microplascs in water and their spaal accumulaon (Barnes et al., 2009). The vast
amounts of anthropogenic debris washing up on beaches across the globe (Browne et al., 2011)
provides visual evidence of the efficiency with which floang plasc debris can be transported on the
sea surface. Approximately half of marine plasc debris is inially buoyant (e.g. polystyrene,
polyethylene, polypropylene), while denser plasc (e.g. polyvinylchloride, nylon) readily sinks in
seawater. As observed from numerous sampling campaigns, microplascs can permeate throughout
the water column, with plasc and microplasc debris, including low‐density polymer plasc, widely
evidentinbenthicecosystems(Milleretal.,inpress).
Laboratory exposures have been used to demonstrate that bioc interacons including
biofouling (Fazey and Ryan, 2016; Kaiser et al., 2017), egeson (Cole et al., 2013; Cole et al., 2016)
and bioturbaon (Näkki et al., 2017), as well as physical processes such as fragmentaon (Andrady,
2017), can affect the properes and movement of plascs; it is hypothesised these processes could
result in changes to the distribuon of microplascs within marine ecosystems where biota and
plascs overlap (Figure 1; Clark et al., 2016). In these waters, we might expect a downwards flux of
plasc debris, resulng in an accumulaon of microplascs on the seafloor (Barnes et al., 2009,
Woodall et al., 2014). However, it is important to recognise that vercal flux should be considered a
redistribuon of plascs, and not a ‘removal’ mechanism. Benthic ecosystems can be highly
biologically‐producve habitats, supporng a diverse array of life that play vital roles in the oceanic
carbon pump (Turner, 2015), reef formaon (Beck et al., 2011) and bioturbaon (Cadee, 1976).
Environmental sampling has idenfied plasc polluon in every benthic habitat invesgated,
including highly remote areas such as both Arcc (Bergmann et al., 2017) and Antarcc (Munari et
al., 2017) polar regions and the deep sea (Woodall et al., 2014, Bergmann et al., 2017). Plasc
concentraons in sediments are highly variable, due in part to different sampling and extracon
methodologies and also to the natural heterogeneity of sediments. Concentraons of up to 6,600
microplascs kg
‐1 have been reported in Arcc sediments (Bergmann et al., 2017) and in a study of 42
sites around the Australian coastline (Ling et al., 2017), a regional average of 3,400 microplascs L
‐1
were reported, with the highest individual sample yielding 12,500 plascs L
‐1
. Laboratory exposures
have shown that benthic invertebrates readily consume plasc, and this can have a detrimental
impact on their health and funconality. A reducon in energy reserves (Wright et al., 2013b),
reproducon (Sussarellu et al., 2016), metabolism and bioturbaon acvity (Green et al., 2016) have
been reported in benthic organisms, with potenal impacts to ecosystem funconing (Volkenborn et
al.,2007).
Figure 1. Potenal pathways for the transport of microplascs and its biological interacons (Source:
Wrightetal.,2013).
Encounteringanddetectionofmicroplastics
Compared to the dynamic interacons between a predator/grazer and their natural prey, the
relaonships between an animal and microplasc is somewhat simplified. The feeding mode and
life‐history of an organism will affect both its encounter and ingeson rate of microplasc. Organisms
may acvely select microplascs from the environment in search of prey or they may ingest them
accidentallywhilefeedingonfoodparclesoranimalswhichcontainplasc.
Apassiveparticle
Microplascs are passive: freely floang on the water surface; suspended or slowly sinking in
the water column; or, deposited on or within the seabed. Encounter rate (i.e. the commonality with
which a predator comes into contact with it’s prey) is a crucial factor affecng the ingeson rate of
that prey (e.g. Evans, 1989). Primarily, encounter rate is influenced by the relave abundance of
predator/grazer and prey; for microplasc ingeson to occur, there would need to be a significant
spaal overlap between biota and plasc, and a substanal amount of plasc present for a likely
encountertooccur.
Classic work on feeding efficiencies have shown how changes in prey density affect the
ingeson rates of predators. Ingeson increases with an increasing prey density up to a saturaon
point, whereby the predator cannot process more prey even though the prey density sll increases,
as described by Solomon (1949) and Holling (1959). This has also been shown in laboratory studies
with virgin microplascs and various invertebrate taxa: the more parcles the organisms were
offered, the more they were ingested, even when working with the relavely high concentraons
used in laboratory sengs (e.g. Cole et al., 2013, Setälä et al., 2016a). Gelanous organisms (e.g.
jellyfish and ctenophores) may feed without reaching a saturaon level. This means that even in very
high concentraons of prey they connue capturing them but start to egest/vomit prey that they are
unable to process. However, it has been observed that jellyfish ingested relavely low numbers of
microplascs compared to other filter feeders (e.g. copepods) in the South China Sea (Sun et al.,
2017). The classical Holling‐type ingeson paerns may also be affected by clogging of feeding
appendages. In such cases, a high concentraon of microplascs (fibres) may decrease feeding
acvity,resulnginloweringesonrates.
Figure 2. Number of ingested 10 µm spheres (mean±SD) in blue mussel (Mytilus trossulus) at three
different bead concentraons (Low = 5, medium = 50 and high = 250 beads mL
‐1
). Source: Setälä et
al.,(2016a).
Acve, mole predators (e.g. cruising predators) will encounter prey, and we therefore assume
plasc, more readily as they move through the water or sediment. Non‐mole animals will encounter
microplascs the same way they come into contact with suspended or deposited prey (i.e. water
currents bringing parcles close enough for capture, or generang localised currents to draw
suspended parcles to the organism). Sessile organisms are also not able to avoid exposure to
microplascs, and are subjected to all parcles present in the suspension they are feeding in.
However, passively floang and sessile organisms, and ambush predators, can compensate for
reducedencounterratesthroughhigh‐efficientfilteringacvity(Greenetal.,2003).
Detectingmicroplastics
Animals detect prey using visual or chemical cues, or hydromechanical signals when idenfying
mole prey moving through the water. Organisms relying upon visual detecon may mistake
microplascs as prey. For example, ocean‐foraging Fulmars travel vast distances across the North
Atlanc, relying on visual cues to select prey floang near the ocean surface; dissecons of Fulmars
beached along European coastlines have rounely idenfied the seabirds’ stomachs are full of plasc
(van Franeker et al., 2011). Researchers oen note that microplasc debris comes in a wide range of
shapes, size and colour, however it is currently unclear whether these aributes have any influence
onitslikelihoodofbeingconsumedbyanimalsrelyingonvisualdetecon.
The swimming acvity and speed of mole prey affects their encounter rate, with numerous
studies establishing that acvely moving prey are detected more frequently and encountered more
oen (Gerritsen & Strickler, 1977, Gerritsen, 1984, Tiselius et al., 1993). As microplascs are passive
parcles, they cannot be detected using hydromechanical signals, and we would therefore expect
them to be encountered less frequently than mole prey at similar concentraons. For example, in
pelagic communies the swimming acvity of the predator is affecng the encounter rate of
microplasc parcles in addion to their density and overall distribuon. However, as plasc
parcles are non‐mole, they make easy targets for predators and may therefore be ingested (if not
acvely rejected) more readily than natural prey which can incite escape‐responses (e.g. Green,
2003),andmayrequireanacvecapturingprocess.
Chemical cues play a significant, but variable role in the prey selecon of marine organisms
from invertebrates to mammals. For example fish have diversely developed olfactory organs (Hara,
1975) for detecng signals related to reproducon and feeding. Some marine species possess highly
developed chemosensory organs (e.g. sharks) while in some others they may be poorly developed,
(e.g. visual predators like pike (Hara, 1975). Crustaceans, such as copepods are generally considered
to be selecve feeders that display flexibility in their feeding behavior (Koehl and Sckler, 1981);
discriminaon between prey can be based on size (Frost 1972), molity (Atkinson 1995) or chemical
signals (Cowles et al.,1988). Not all chemicals are sensed; what is important is that in order for an
organism to receive a chemical smuli, the chemical itself should be soluble in water. Chemical
signals can assist in the selecon for high‐quality food, determined by protein content (Cowles et al.,
1988), or be used to avoid unsuitable prey (e.g. harmful algae containing toxic compounds like
saxitoxin). However, acve avoidance of unsuitable or toxic prey by copepods is most likely a result of
acommonhistory,i.e.co‐evoluonofthepreyandpredator(Colin&Dam,2002).
Field‐collected data and exposure experiments show that plasc parcles floang in the
water and embedded in the sediment are rapidly colonized by rich microbial communies comprising
of procaryoc and eucaryoc organisms, like bacteria and algae (Oberbeckmann et al., 2014,
Harrison et al., 2014). So far there is very lile informaon on how the formaon of biofilm actually
affects the ingeson of microplascs. Recent studies show, that the effects of biofouling are most
likely taxon‐ or even species‐specific. Vroom et al., 2017 idenfied that biofouling of polystyrene
beads promoted ingeson by planktonic crustaceans, although this was somewhat dependent on
taxon, size and stage of the grazers. For two of the three copepod species studied (Acartia longiremis
and Calanus finmarchicus, excluding the adult females of the laer) it was shown that in most cases
the fouled microplascs were ingested by more individuals and at higher rates than the unfouled
plascs. However one copepod species, Pseudocalanus spp., did not ingest any of the microplasc
parcles offered. Contradictory results were reported by Allen et al., (2017) who studied the
ingeson of weathered, fouled and unfouled pre‐producon pellets (PS, LDPE and HDPE), by a
scleracnian coral species known to use chemosensory cues for feeding. Their results showed that
the corals ingested different types of plascs, consuming significantly more unfouled than fouled
microplascsweretakenup.
INFOBOX2:Experimentalwork
Most of the informaon that has so far been produced on the parameters affecng microplasc
ingeson by marine organisms come from simplified laboratory experiments. Results from
experimental work should not be directly applied to natural condions where confounding factors
exist. When conducng environmentally relevant experimental work on ingeson and effects of
microplascs in food webs, the concentraon, size and type of the used parcles should be adjusted
to correspond to natural condions. At the moment there is sll a mismatch between “reality” and
laboratory experiments. So far most experiments are run with microplasc concentraons higher
than those commonly found in the environment, and with virgin parcles of uniform size and shape
that fail to accurately represent the condions in the field (Phuong et al., 2016). This inconsistency is
likely to influence our understanding of the marine microplasc problem as Ogonowski et al., (2016)
showed in laboratory experiments comparing the effects of primary and secondary microplascs.
They showed that secondary microplascs have more negave effects on feeding in a cladoceran,
Daphnia magna,compared to primary microplascs commonly used in previous studies. The reason
why experimental laboratory studies have not used microplasc concentraons commonly observed
in marine environment is their “low” concentraons but also the uncertainty in assessing their
concentraons. Microplasc concentraons found in marine environments vary significantly
between areas and habitats but seem to be low when compared to the numbers of the real prey,
which makes environmentally relevant exposure studies difficult. Long lasng exposure experiments
in mesocosms mimicking natural condions would be needed to more accurately assess the
relaonshipsbetweenmicroplascsandtheirpotenalpredators.
Intothefoodwebs
The ingeson, entanglement or inhalaon of microplasc by marine organisms can be viewed
as an entry point into marine food webs. Owing to their small size, microplascs are bioavailable to a
wide range of marine organisms, and can be both selecvely and accidentally ingested (Schuyler et
al., 2012). The ingeson of microplasc parcles is affected by their concentraon, size, shape,
distribuon and chemical character (i.e. density, chemical signal), and the animal’s feeding habits. In
animals with developed organs for prey detecon, plasc polymers may thus not be selected or they
mayberejectediftheyarerecognizedasbeingunfavorable,orifamorepreferablepreyisavailable.
Filterfeeding
Filter feeding organisms are prevalent throughout marine food webs, from small planktonic
invertebrates and benthic taxa, to megafauna, where they feed on suspended organic material, such
as algae, zooplankton, fish larvae and detritus. The size range of parcles that can be ingested by a
grazer depends on the feeding mode (e.g. filter feeding or raptorial), gape size and specific feeding
mechanisms of the grazer/predator. For filter feeders, the actual size limits for the ingested prey are
set by the structure and funcon of the filtering apparatus used for trapping parcles from the
suspension (Riisgård and Larsen, 2010). Filtering devices in suspension feeding organisms are not
simple sieves that mechanically clean the water from suspended parcles. The structures of filtering
apparatus found in unicellular, invertebrate or vertebrate organisms differ greatly, both between and
among taxa, with varying levels of adaptability and sensory capability. Parcle capture depends on
parcle type (e.g. shape, size, density), parcle concentraon, water viscosity, the quanty of water
that is filtered and filtering efficiency. Besides direct contact, the capturing mechanisms may also
involve other factors, such as chemo‐ and mechanorecepon (Riisgård and Larsen, 2010). Moreover,
experimentally measured clearance rates of plankton have been found to vary also depending on
temperature, salinity and the type of prey that has been offered (e.g. Kiorboe, 1982, Garrido et al.,
2013). Daily clearance rates of marine invertebrates can vary from microlitres (unicellular organisms,
like ciliates), to millilitres (copepods), litres (bivalves), hundreds of litres (gelanous zooplankton), or
more(baleenwhales).
Two parameters are commonly used to esmate the efficiency and outcome of filter feeding:
ingeson and clearance rate. The ingeson rate denotes the number of prey parcles ingested per
predator in a me unit. Ingeson rate can be experimentally esmated directly, through observaons
of ingested prey parcles inside the organism, or indirectly, as the disappearance of prey from the
experimental media over me. In the past, inert plasc parcles (spheres) have been used as
surrogates for natural prey to esmate feeding parameters in planktonic organisms (Huntley et al.,
1983, Borsheim, 1984, Nygaard et al., 1988,). These historical studies with Calanus and related
copepod genera have demonstrated a preference for algae over polystyrene beads, alongside size
selecvity (Fernandez 1979, Donaghay and Small, 1979, Huntley et al., 1983). However, observaons
for such preferences do not necessarily hold for all developmental stages, which further complicates
things, i.e. when exposure studies are being conducted. Clearance rate is a derivave of ingeson
rate and is calculated by dividing the laer by prey concentraon. The clearance rate thus measures
the water volume that an individual organism can clear of food parcles in a me unit. To understand
the probability of any suspended parcle to be ingested by a filter feeding organism, both the
clearancerateandtheconcentraonofsuitablepreyshouldbetakenintoaccount.
From the viewpoint of a small filter‐feeding organism under natural condions, microplasc
concentraons may be too low for rounely encountering a plasc parcle. However, in waters
containing high concentraons of microplascs the situaon is different even for a small organism
with a relavely low clearance rate and efficiency, such as a copepod. As an example, the
experimentally defined daily clearance rates of common copepods may vary between ca. 10 to <200
mL (Frost, 1975, Engström et al., 2000, Setälä et al., 2009). In theory, a copepod feeding for example
with a high clearance rate of 144 mL / day (Frost, 1975), at a concentraon of 9200 plascs m
‐3 as has
been observed from the Pacific Ocean (Deforges et al., 2014), a single microplasc would be ingested
by every 0.7 copepods, assuming all parcles are edible and the animals are solely undertaking
passive ingeson without rejecon of plasc. Assessments based on animals collected from the field,
have also confirmed the role of zooplankton as entry points for microplascs to food webs. In the
study of Desforges et al., (2015) which was based on analysis of the number of ingested microplascs
from subsurface collected zooplankton and the overall distribuon of these species from the
Northeast Pacific Ocean idenfied encounter of microplascs by zooplankton as 1 parcle per every
34 copepods and 1 parcle per every 17 euphausiid. The authors further esmated that both the
juvenile salmon as well as adult returning fish would be affected daily with ingested microplascs
throughtheirzooplanktonprey.
Invertebrates with capacity for filtering larger quanes of water, and with a longer lifespan
(e.g. bivalves), or large filter feeders (such as whales) may encounter microplascs far more
frequently than zooplankton. Bivalves are one of the key organisms when entry points of
microplascs to marine food webs are assessed. They are efficient suspension feeding animals that
form links between the pelagic and benthic ecosystems and are a key source of prey for many marine
fish, birds and mammals. In the Balc Sea it has been assessed that within one year the blue mussel
beds would, in theory, filter a water volume equivalent to the whole sea basin (Kautsky and Kautsky,
2000). The numbers of microplascs found in bivalves vary significantly ranging from less than 0.5
parcles (Eastern Atlanc and Balc Sea) to over 100 parcles (Western Atlanc) per animal
(Mathalon and Hill, 2014, Vandermeersch et al., 2015, Railo, 2017). Exposure of large filter feeders to
microplascs has been shown by Fossi et al., (2014) aer examining concentraons of phthalates and
organochlorine compounds of a basking shark and a baleen whale. The authors concluded that
micro‐lier is ingested by these large filter feeders together with their neustonic prey. A comparave
study carried out in two semi‐enclosed basins; the Mediterranean Sea and the Sea of Cortez in the
Gulf of California (Fossi et al., 2016) gives supporng informaon indicang that fin whales in highly
polluted areas are exposed to major health hazards due to microplascs and their co‐contaminants.
Considering the vast amounts of water these animals filter (5,893 m
3
/day; Fossi et al., 2014), this
conclusionismorethanrelevant.
INFOBOX3:Microplastics,anissueofsize
‘Microplasc’ is typically used to describe plasc parcles smaller than 5 mm in diameter, with
a lower size limit of 100 nm; plascs larger than 5 mm are considered ‘macroplascs’, while plascs
smaller than 100 nm in size are termed ‘nanoplasc’ (Cole et al., 2011). Using these size
classificaons, the largest microplasc parcles (5000 µm) have a diameter 50,000 mes larger than
the smallest microplasc (0.1 µm). Moreover, when we consider volume and surface area, these
differences become even more apparent. Imagine a spherical shaped microplasc parcle, like the
ones used in experimental studies, or the plasc microbeads commonly used in exfoliang personal
care products: a 5 mm diameter bead is 1.25 x 10
14
mes greater in volume and 2.50 x 10
9larger by
area than a 100 nm diameter bead. Of course most of the weathered microplasc parcles that are
found in the marine environment are not uniform in shape, with fibrous, planar and irregularly
shaped plasc being most prevalent. Nevertheless, differences in a parcle’s dimensions will have a
significant impact on the risk they pose to marine life. For example, microplascs of different sizes
may differ in their behaviour under marine condions (i.e. buoyancy), biological availability, and
capacity to incite biological effects. Furthermore, the larger surface area to volume raos associated
with smaller parcles greatly increases the plasc’s capacity for adsorbing (and potenally
desorbing) water borne pollutants (e.g. persistent organic pollutants, hydrophobic organic
contaminants) (Koelmans et al., 2016), up to one million mes greater than that found in the
surroundingseawater(Matoetal.,2001)
Respiratoryintake
Venlaon has also been idenfied in exposure experiments as a means by which microplascs
can be concentrated from the surrounding water. Was et al., (2014) idenfied that the shore crab
(Carcinus maenas) was able to respire polystyrene microbeads, which accumulated on the surface of
their gills. Blue mussels (Mytilus trossulus) and Balc clams (Macoma balthica) have also been shown
to accumulate microplasc parcles to their gills aer 24 h incubaons; however, the bead
concentraonsweremuchhigherinthedigesvetractsofthesameanimals(Setäläetal.,2016a).
Entanglement
Numerous organisms have been shown to entangle with fibers or larger plascs (e.g. Laist,
1997, Cole et al., 2013, NOAA 2014, Taylor et al., 2016). They may be found in the swimming or
feeding appendages of invertebrates, in the valve gapes of bivalves or entangled around larger
animals. Entanglement with fibers in field collected animals has been observed even in remote areas
such as the deep seas, where fibers were found on sea pens and hermit crabs (Taylor et al., 2016).
When these organisms are eaten by higher trophic level predators the plascs adhered to external
surfacesoftheorganismswillbeeatenaswell.
Trophictransfer
Once ingested, microplascs will either be egested or retained by the organism. If a predator
consumes an organism that has retained microplasc, the predator will be indirectly consuming this
plasc as part of its diet, in a process referred to as ‘trophic transfer’. The trophic transfer of plasc
has been documented in predatory Norway lobsters (Nephrops norvegicus) that consumed
polypropylene rope fibres embedded in fish (Murray and Cowie, 2011); shores crabs (Carcinus
maenas) that indirectly ingested fluorescent polystyrene 0.5 µm and 10 µm microspheres present in
common mussels (Mytilus edulis) (Farrell and Nelson, 2013; Was et al., 2014); mysid shrimps
(Neomysis integer) that consumed fluorescent polystyrene 10 µm spheres previously taken up by
mesozooplankton (Setälä et al., 2014); and, fish (Gasterosteus aculeatus) that consumed an insect
larvae containing microbeads in a mesocosm experiment (Lehniemi and Setälä, unpublished). The
trophic transfer of microplascs and associated POPs from Artemia nauplii to zebrafish (Danio rerio)
was also verified in a laboratory experiment (Batel et al., 2016) and microplasc debris found in
faecal pellets of predatory seabirds (great skuas, Stercorarius skua) was greatest when correlated
withremainsofsurfacefeedingNorthernfulmars(Fulmarusglacialis)(Hammeretal.,2016).
For trophic transfer to occur, microplasc must be consumed alongside the prey. This includes
plasc adhered to algae (Bhaacharya et al., 2010, Gutow et al., 2015), or the external surfaces of an
animal (e.g. entrapped in the setae of a copepods’ appendages; Cole et al., 2013), or retained
indefinitely within the organism itself. Plascs are commonly observed in the intesnal tract of
marine animals, including seabirds (van Franeker & Law, 2015), fish (Lusher et al., 2013),
invertebrates (Murray and Cowie, 2011) and turtles (Nelms, 2016); this occurs where larger plascs
or coalesced polymeric fibres cause a gut blockage, prevenng the plasc from being shied via
peristalc acon. In the common shore crab (Carcinus maenas), polystyrene microspheres have been
observed to lodge between the microvillae which line the stomach, resulng in prolonged gut
retenon mes. In copepods, starvaon has been observed to increase gut retenon mes, with 10
µm polystyrene microspheres remaining in the intesnal tracts of Calanus helgolandicus for up to 7
days, far exceeding the typical gut passage mes of just 2 hours (Cole et al., 2013). In the common
mussel (Mytilus edulis), 3.0‐9.6 µm polystyrene microspheres have been demonstrated to translocate
into the circulatory fluid (haemolymph), where they can remain for in excess of 48 days (Browne et
al., 2008; von Moos et al., 2012). Owing to their small size, nanoplascs (<100 nm diameter) have the
capacity to cross epithelia, and therefore have the capacity to enter ssues and circulatory fluids, for
example in dendric cells that transport small parcles (eg. bacteria) across gut epithelial cell walls
(Rescignoetal.,2001).
In numerous aquac ecosystems, persistent chemical pollutants (i.e. PCBs, PAHs and methyl
mercury) have been shown to biomagnify as they pass up the food chain (reviewed by Blais et al.,
2007). The increasing body burdens of such pollutants in higher trophic organisms arises from the
hydrophobicity of these chemicals, resulng in their accumulaon within fay ssues of prey
species. So far, there have been no quantave measures of microplascs passing up the food chain,
and it therefore remains unclear whether plascs will biomagnify in marine food webs.
Biomagnificaon will largely depend upon the transience of plascs in an organism, with
biomagnificaon only occurring where plascs are readily ingested and retained. Retenon of
plascs can be influenced by food availability (Cole et al., 2013; Was et al., 2014) and shape (Murray
and Cowie, 2001), but will be predominantly governed by the size of the plasc (Galloway, 2015). In
Figure 3. we predict how the size of a plasc parcle is likely to relate to the probability of that
microplascbiomagnifyingupthefoodchain.
Figure 3. Considering how microplasc size might influence the probability of biomagnificaon of
plascs occurring in a food chain. (1) Very small (i.e. nano) plascs are readily absorbed by the gut
and are retained within the circulatory fluid and/or ssues; (2) Moderately sized plascs are ingested,
are present within the organism during gut transit, and then readily egested; (3) Larger and fibrous
plascs are ingested but, owing to their size, remain in the intesnal tract; (4) The largest
microplascsareinedibletoorganismsatthebaseofthefoodchain.
Alteration,repackagingandtransportofmicroplasticswithinmarinefoodwebs
In this secon, we consider how marine organisms, trophic dynamics and biologically‐mediated
ecological processes can alter the fate of a microplasc, and highlight how microplascs might
impingeonbiota,foodwebsandthemarineecosystems.
Biologicaltransportofmicroplastic
Microplascs consumed, respired or adhered by an organism will be subject to passive,
biologically‐mediated transportaon, with both vercal and lateral movement to be expected across
a variety of habitats (e.g. water column, sediments). The distances by which microplascs can be
transported via a biological vector will largely depend on the movement, migratory routes and gut
transitmesoftheindividualorganism.
Figure 4. How biota transport microplascs within marine ecosystems. Image by Mahew Cole
(originalcontent).
Diel vercal migraons, a synchronous daily migraon of a wide range of taxa, have been
highlighted as a potenal route by which microplascs could be transported from the sea surface to
deeper waters (Cole et al., 2016b; Clark et al., 2016). Organisms may ingest plascs whilst feeding at
the surface at night, which can then be egested hundreds of meters below the surface. For example,
a large (2‐3 mm) copepod swimming at speeds of between 30–90 m h
‐1 (Enright, 1977), with a gut
evacuaon me of approximately 2 hours (Cole et al., 2013), could vercally transport microplasc to
depths of 60‐180 m. Lusher et al., (2016) idenfied that 11% of mesopelagic fish caught in the
Northeast Atlanc had microplascs in their digesve tracts, and although it was unknown at what
depth these plascs were consumed, the majority of species idenfied undergo diel vercal
migraon and follow their zooplankton prey to the surface to feed; it is therefore plausible to suggest
that ingeson of the microplascs may have occurred at the surface whilst feeding, and egested at
depth.
The geographical distribuon of marine plasc has largely been considered from a physical
perspecve, with abioc processes (i.e. wind, rivers, oceanic currents) expected to be the dominant
factors in distribung this pervasive pollutant (Sherman and van Sebille, 2016). We consider that
migratory species could also facilitate the transport of plascs. Migratory species have been widely
demonstrated to play a vital role in the long‐range transport of persistent pollutants (e.g. PCBs, DDT,
methyl mercury; Blais et al., 2007). For example, migratory fish (e.g. trout, salmon) have been shown
to accumulate persistent organochlorines in their ssues while feeding in marine habitats, which are
released in their eggs during spawning at otherwise prisne, freshwaters sites (Krummel et al., 2003;
Mu et al., 2004). Numerous migratory species, including turtles (Nelms et al., 2015), ocean‐foraging
seabirds (van Franeker, 2015), and cetaceans (Lusher et al., 2015), are rounely sampled with plascs
in their intesnal tracts. These animals undertake large scale, annual migraons; for example, the
Gray whale (Eschrichtius robustus) travels 6000 km annually from the coast of Mexico to the Chukchi
Sea, and the Arcc tern (Sterna paradiasaea) migrates 19,000 km from Greenland to the Antarcc
each year (Alerstam et al., 2003). The egeson of plasc within faeces, scat or guano, the
regurgitaon of plascs by seabirds when feeding their young (Sileo et al., 1990), or the death of the
animal, will all contribute to the deposion of plasc in terrestrial, freshwater or marine habitats far
fromthewaterswheresuchplascwasingested.
Incorporationofmicroplasticsintobiologicalmatrices
Within the marine environment, microplascs are rapidly colonized by ‘biofilms’, made up of
microorganisms, plants and epibionts that aach and grow on substrates. The characteriscs of the
biofilm that forms on a plasc will be influenced by the polymer, and the biological or ecological
matrix through which it has passed; as such, the microbial complex that forms on the surface of
plascs may act as a tracer of the journey of a microplasc within marine compartments (Galloway
et al., 2017). The development of a biofilm can change the characteriscs of the plasc polymer, for
example by increasing their mass (Lobelle and Cunliffe, 2011; Zeler et al., 2013; Rummel et al.,
2017), and altering their chemical signal (see Detecting microplastics). It has been postulated that
biofilm formaon could be enough to cause otherwise buoyant plascs to sink or oscillate within the
water column, depending on the size and density of the plasc (Ye & Andrady, 1991, Kooi et al.,
2017).
In bivalves, feeding or rejecon of parcles that are suspended in the water is the outcome of
passive and acve selecon. The size of the parcles that may be ingested depends on the filtraon
apparatus of the parcular species. In Pacific oyster (Crassostrea gigas) larvae, uptake of polystyrene
microbeads was size dependent, with microplascs larger than the oral groove unable to be ingested,
while smaller plascs were readily consumed (Cole & Galloway, 2015). If the size is right, and prey is
directed to the specialized feeding organs (ctenidium) it may sll be rejected as pseudofaeces if
considered unpalatable. Studies made with blue mussels have shown that the idenficaon of
unsuitable parcles and their sorng in suspension‐feeding bivalves takes place in the
lecn‐containing mucus that covers feeding organs, where interacon with carbohydrates from
suspension takes place (Espinosa et al., 2010). Mussels (Mytilus edulis) have been visualised rejecng
nanopolystyrene (Ward & Koch, 2009), and microplasc polyvinylchloride in their pseudofaeces
(personal observaons of authors). The fate of microplascs incorporated into pseudofaeces remains
unclear.
Ingested microplascs will typically be passed along the intesnal tract through peristalc
acon. Within the intesnal tract microplascs will either be adsorbed across the gut lining, become
entrapped in the gut (i.e. intesnal blockage causing retenon of plasc), or become incorporated
into the animal’s faeces and egested. Microplascs have been idenfied in the faecal pellets of
copepods (Cole et al., 2013), and it is assumed most animals that consume plascs will then egest
them. Microplascs have been observed in commercially caught fish (e.g. Lusher et al., 2013), and
whilst there is currently no data to explain the fate of plasc post ingeson, it could be assumed that
the majority would pass through the gut and get packaged in faecal pellets. The repackaging of
plasc into the faeces of an animal will alter the properes (i.e. relave buoyancy) of the plascs
within the water column (Cole et al., 2015), and represent an alternate route by which plascs can be
transferredwithinmarineecosystems(Clarketal.,2016).
Sinking faeces and marine aggregates play a vital role in the biological pump, whereby carbon
and nutrients in the euphoc zone are repackaged, and transported to the ocean depths (Turner,
2014). Faeces from anchovies in the producve upwelling system off the coast of Peru were observed
as a key contributor to downward flux in sediment traps, with faecal sinking rates averaging >1 km d
‐1
(Staresinic et al., 1983). In this scenario, any microplascs contained within these pellets may reach
benthic sediments within a very short space of me. However, experimental work has documented
that the incorporaon of microplascs into faecal pellets (Cole et al., 2016) and marine aggregates
(Long et al., 2015), will alter the buoyancy of the biological matrix. Many carbon flux studies have
concluded that slowly sinking faeces are unlikely to reach the seabed, instead becoming repackaged
through coprophagy (i.e. the consumpon of faecal maer) by larger zooplankton species (Turner,
2002), or broken down through microbial acon. In faeces containing microplasc, coprophagy
would therefore represent a route by which plascs can re‐enter the marine food web. This has been
demonstrated with copepods, when polystyrene microplascs ingested by the small copepod,
Centropages typicus, were egested in their faecal pellets and subsequently ingested by the larger
copepod, Calanus helgolandicus (Cole et al., 2016). The study further highlighted that
microplasc‐laden pellets were more prone to fragment, making them more bioavailable to
detrivoresduringtheirdescentthroughthewatercolumn.
Thefateofmicroplasticsinbenthicecosystems
Benthic sediments have been idenfied as an important sink for microplascs, including high‐density
plascs which readily sele out of the water column, and lower‐density plascs whose movement to
the benthos is facilitated by biological matrices. Highly polluted coastal sediments may comprise 3%
microplascs (Carson et al., 2011), whilst esmates of 4 billion bioplasc and polymer fibres per km
2
are reported in Indian seamount sediments (Woodall et al., 2014). Within sediments, microplascs
become bioavailable to benthic dwelling fauna, including important commercial species such as
Norwegian lobster, Nephrops norvegicus (Murray & Cowie, 2011) and shellfish (Rochman et al.,
2015). A number of papers having highlighted the capacity for benthic organisms, including bivalves
(Sussarellu et al., 2016), echinoderms (Graham & Thompson, 2009) and polychaetes (Wright et al.,
2013, Besseling et al, Green et al., 2016) to ingest microplascs, with the potenal to incite negave
health effects with repercussions for their funconality (i.e. reduced bioturbaon acvity, reduced
energec reserves). As with pelagic organisms, it is hypothesised that benthic taxa can alter the
properes of microplascs, and through bioturbaon move plascs from the sediment‐water
interface deeper into sediments. This has been evidenced in polychaetes and clams that transported
microplasc fibres (polyethylene fishing line <1 mm) to depths of 1.7‐5.1 cm during a three week
mesocosm experiment (Näkki et al., 2017). However, determining the capacity for sediment‐dwelling
biota to redistribute plasc under natural condions remains unknown, and it is unclear whether
bioturbaoncanresultinthepermanentburialofthisplasc.
Conclusions
Microplascs are under extensive research, and their complex interacons with marine food webs
are becoming increasingly evident. Microplascs are pervasive, environmentally‐persistent parcles,
which have the potenal to flux between the water column, seabed and biota. Nano‐ and
microplascs can enter marine food webs via a number of entry‐points, and can subsequently be
cycled through different bioc compartments; these bioc processes can result in changes to the
properes and movement of the microplasc. Parameters governing the entrance of microplascs
into food webs include the spaal overlap of microplascs and biota, the feeding strategy and
molity of the organism, and the characteriscs of the plasc. From the studies carried out so far, we
have learned that different taxa, species, and developmental stage of a species, will each process,
handle and react to microplascs in a myriad of ways. Some organisms have mechanisms that
protect them from consuming anthropogenic contaminants, while others readily ingest large
numbers of microplasc parcles together with their natural prey. With microplasc polluon in the
marine environment becoming a growing threat, the numbers of both primary‐ and secondary
microplascs is increasing. There may therefore come a me, when the exposure experiments which
are carried out today, and which have been cricized because of their high microplasc
concentraons, will be considered as “historic” research with environmentally relevant
concentraons.
Funding
OS and ML acknowledge Ministry of Environment and Academy of Finland (MIF 296169) for funding.
RLC is funded through a Natural Environment Research Council GW4+ PhD studentship
(NE/L002434/1). MC acknowledges funding from the Natural Environment Research Council
discoverygrant(NE/L007010).
References
Allen, A.S., Seymour, A.C. & Rischof, D. (2017). Chemorecepon drives plasc consumpon in a
hardcoral.MarinePollutionBulletin.124(1),198‐205.
Alerstam, T. Hedenström, A., & Åkesson, S. (2003). Long‐distance migraon: evoluon and
determinants.Oikos.103(2),247‐260.
Andrady, A.L. (2017). The plasc in microplascs: A review. Marine Pollution Bulletin. 119(1),
12–22.
Atkinson, A. (1995). Omnivory and feeding selecvity in five copepod species during spring in the
BellingshausenSea,Antarcca.ICESJournalofmarineScience.52(3‐4),385‐396.
Barnes, D.K., Galgani, F., Thompson, R.C., & Barlaz, M. (2009). Accumulaon and fragmentaon of
plasc debris in global environments. Philosophical Transactions of the Royal Society of
London.SeriesB,BiologicalSciences.364(1526),1985–1998.
Batel, A., Lin, F., Scherer, M., Erdinger, L., & Braunbeck, T. (2016). The transfer of benzo [a] pyrene
from microplascs to Artemia nauplii and further to zebrafish via a trophic food web
experiment–CYP1A inducon and visual tracking of persistent organic pollutants.
EnvironmentalToxicologyandChemistry.35(7),1656–1666.
Beck, M.W., Brumbaugh, R.D., Airoldi, L., Carranza, A., Coen, L.D., Crawford, C., Defeo, O., Edgar,
G.J., Hancock, B., Kay, M.C. & Lenihan, H.S. (2011). Oyster reefs at risk and recommendaons
forconservaon,restoraon,andmanagement.Bioscience.61(2),107‐116.
Bellas, J., Marnez‐Armental, J., Marnez‐Camara, A., Besada, V. & Marnez‐Gomez, C. (2016).
Ingeson of microplascs by demersal fish from the Spanish Atlanc and Mediterranean
coasts.MarinePollutionBulletin.109(1),55‐60.
Bergmann, M., Wirzberger, V., Krumpen, T., Lorenz, C., Primpke, S., Tekman, M.B. & Gerdts, G.
(2017). High quanes of microplasc in Arcc deep‐sea sediments from the HAUSGARTEN
observatory.EnvironmentalScience&Technology.51(19),11000‐11010.
Besseling, E., Wegner, A., Foekema, E.M., Van Den Heuvel‐Greve, M.J. & Koelmans, A.A. (2012).
Effects of microplasc on fitness and PCB bioaccumulaon by the lugworm Arenicola marina
(L.).EnvironmentalScience&Technology.47(1),593‐600.
Bhaacharya, P., Lin, S., Turner, J.P. & Ke, P.C. (2010). Physical adsorpon of charged plasc
nanoparcles affects algal photosynthesis. The Journal of Physical Chemistry C: Nanomaterials
andInterfaces.114(39),16556.
Blais, J.M., Macdonald, R.W., Mackay, D., Webster, E., Harvey, C. & Smol, J. P. (2007). Biologically
mediated transport of contaminants to aquac systems. Environmental Science & Technology.
41(4),1075‐1084.
Borsheim, K. Y. (1984). Clearance rates of bacteria sized parcles by freshwater ciliates measured
withmonodispersefluorescentlatexbeads.Oecologia(Berlin).63,286−288.
Bravo Rebolledo, E.L., Van Franeker, J.A., Jansen, O.E. & Brasseur, S.M. (2013). Plasc ingeson by
harbourseals(Phocavitulina)intheNetherlands.MarinePollutionBulletin.67,200–202.
Bråte, I.L.N., Huwer, B., Thomas, K.V., Eidsvoll, D.P., Halsband, C., Carney Almroth, B. & Lusher, A.
(2017). Micro‐and macro‐plascs in marine species from Nordic waters. Nordic Council of
Ministers.101p,48‐49.DOI:10.6027/TN2017‐549
Browne, M.A., Dissanayake, A., Galloway, T.S., Lowe, D.M. & Thompson, R.C. (2008). Ingested
microscopic plasc translocates to the circulatory system of the mussel, Mylus edulis (L.).
EnvironmentalScience&Technology.42(13),5026‐5031.
Browne, M.A., Crump, P., Niven, S.J., Teuten, E., Tonkin, A., Galloway, T.S. & Thompson, R.C.
(2011). Accumulaon of microplasc on shorelines worldwide: sources and sinks.
EnvironmentalScience&Technology.45(21),9175‐9179.
Budimir, S., Setälä, O. & Lehniemi, M. (in press). New praccal and affordable extracon method
shows low numbers of microplascs in offshore plankvorous fish from the northern Balc
Sea.MarinePollutionBulletin.
Cadée, G.C. (1976). Sediment reworking by Arenicola marina on dal flats in the Dutch Wadden
Sea.NetherlandsJournalofSeaResearch.10(4),440‐460.
Carson, H.S., Colbert, S. L., Kaylor, M. J. & McDermid, K.J. (2011). Small plasc debris changes
water movement and heat transfer through beach sediments. Marine Pollution Bulletin. 62,
1708−1713.
Clark, J., Cole, M., Lindeque, P. K., Fileman, E., Blackford, J., Lewis, C., Lenton, T.M. & Galloway, T. S.
(2016). Marine microplasc debris: a targeted plan for understanding and quanfying
interaconswithmarinelife.FrontiersinEcologyandtheEnvironment.14(6),317–324.
Cole, M., Lindeque, P., Halsband, C., & Galloway, T. S. (2011). Microplascs as contaminants in the
marineenvironment:Areview.MarinePollutionBulletin.62(12),2588–2597.
Cole, M., Lindeque, P., Fileman, E., Halsband, C., Goodhead, R., Moger, J. & Galloway, T.S. (2013).
Microplascingesonbyzooplankton.EnvironmentalScience&Technology.47,6646‐6655.
Cole, M. & Galloway, T.S. (2015). Ingeson of nanoplascs and microplascs by Pacific oyster
larvae.EnvironmentalScience&Technology.49,14625–14632
Cole, M., Lindeque, P., Fileman, E., Halsband, C., Galloway, T.S. (2015). The impact of polystyrene
microplascs on feeding, funcon and fecundity in the marine copepod Calanus helgolandicus.
EnvironmentalScience&Technology.49(2),1130‐1137.
Cole, M., Lindeque, P. K., Fileman, E., Clark, J., Lewis, C., Halsband, C., & Galloway, T. S. (2016).
Microplascs Alter the Properes and Sinking Rates of Zooplankton Faecal Pellets.
EnvironmentalScience&Technology.50(6),3239–3246.
Colin, S.P. & Dam, H.G. (2002). Effects of the toxic dinoflagellate Alexandrium fundyense on the
copepod Acartia hudsonica: a test of the mechanisms that reduce ingeson rates. Marine
EcologyProgressSeries.248,55‐65.
Collignon, A., Hecq, J. H., Galgani, F., Voisin, P., Collard, F., & Goffart, A. (2012). Neustonic
microplasc and zooplankton in the North Western Mediterranean Sea. Marine Pollution
Bulletin.64(4),861‐864.
Cowles T.J., Olson R.J. & Chisholm S.W. (1988). Food selecon by copepods: discriminaon on the
basisoffoodquality.MarineBiology.100,41‐49.
Cózar, A., Sanz‐Marn, M., Mar, E., González‐Gordillo, J.I., Ubeda, B., Gálvez, J.Á., Irigoien, X. &
Duarte, C.M. (2015). Plasc accumulaon in the Mediterranean Sea. PLoS One. 10(4)
.e0121762.
Desforges, J.P.W., Galbraith, M., Dangerfield, N. & Ross, P.S. (2014). Widespread distribuon of
microplascs in subsurface seawater in the NE Pacific Ocean. Marine Pollution Bulletin. 79,
94e99.
Desforges, J.P.,W., Galbraith, M. & Ross, P.S. (2015). Ingeson of Microplascs by Zooplankton in
the Northeast Pacific Ocean. Archives of Environmental Contamination and Toxicology. 69(3),
320–330.
Donaghay, P.L. & Small, L.F. (1979). Food selecon capabilies of the estuarine copepod Acartia
clausi.MarineBiology.52,137e146.
Do Sul, J.A.I., Costa, M.F. & Fillmann, G. (2014). Microplascs in the pelagic environment around
oceanic islands of the Western Tropical Atlanc Ocean. Water, Air & Soil Pollution. 225(7) 2004.
doi.org/10.1007/s11270‐014‐2004‐z
Devriese, L.I., van der Meulen, M.D., Maes, T., Bekaert, K., Paul‐Pont, I., Frère, L., Robbens, J. &
Vethaak, A.D. (2015). Microplasc contaminaon in brown shrimp (Crangon crangon, Linnaeus
1758) from coastal waters of the Southern North Sea and Channel area. Marine pollution
Bulletin.98(1),179‐187.
Engström, J., Koski, M., Viitasalo, M., Reinikainen, M., Repka, S., & Sivonen, K. (2000). Feeding
interacons of the copepods Eurytemora affinis and Acartia bifilosa with the cyanobacteria
Nodulariasp.JournalofPlanktonResearch.22(7),1403‐1409.
Enright, J. T. (1977). Copepods in a hurry: Sustained high‐speed upward migraon. Limnology &
Oceanography.22,118–125.
Eriksen, M., Maximenko, N., Thiel, M., Cummins, A., Lan, G., Wilson, S., Hafner, J., Zellers, A. &
Rifman, S. (2013). Plasc polluon in the South Pacific subtropical gyre. Marine Pollution
Bulletin.68(1),71‐76.
Eriksen, M., Lebreton, L.C.M., Carson, H.S., Thiel, M., Moore, C.J., Borerro, J.C., Galgani, F., Ryan,
P.G. & Reisser, J. (2014). Plasc polluon in the world's oceans: 5 trillion plasc pieces weighing
over250.000tonsafloatatsea.PLoSOne.9(12),1‐15.DOI:10.1371/journal.pone.0111913
Espinosa, E.P., Hassan, D., Ward, J.E., Shumway, S. & Allam, B. (2010). Role of Epicellular Molecules
intheSeleconofParclesbytheBlueMussel,Mytilusedulis.BiologicalBulletin.219,50‐60.
Evans, G.T. (1989). The encounter speed of moving predator and prey. Journal of Plankton
Research.11,415‐417.
Farrell P. & Nelson, K. (2013). Trophic level transfer of microplasc: Mytilus edulis (L.) to Carcinus
maenas(L.).EnvironmentalPollution.177,1–3.
Fazey, F.M. & Ryan, P.G. (2016). Biofouling on buoyant marine plascs: An experimental study into
theeffectofsizeonsurfacelongevity.EnvironmentalPollution.210,354‐360.
Fernandez, F. (1979). Parcle selecon in the nauplius of Calanus pacificus. Journal of Plankton
Research.1(4),313‐328.
Fossi, M.C., Coppola, D., Baini, M., Gianne, M., Guerran, C. & Marsili, L. (2014). Large filter
feeding marine organisms as indicators of microplasc in the pelagic environment: the case
studies of the Mediterranean basking shark (Cetorhinus maximus) and fin whale (Balaenoptera
physalus).MarineEnvironmentalResearch.100,17‐24.
Fossi, M.C., Marsili, L., Baini, M., Gianne, M., Coppola, D. & Guerran, C. (2016). Fin whales and
microplascs: the Mediterranean Sea and the Sea of Cortez scenarios. Environmental Pollution.
209,68–78.
Frost, B.W. (1972). Effects of size and concentraon of food parcles on the feeding behaviour of
themarineplanktoniccopepodCalanuspacificus.Limnology&Oceanography.17,805‐815.
Galgani,F.,Hanke,G.,Werner,S.D.V.L.&DeVrees,L.(2013).MarinelierwithintheEuropean
marinestrategyframeworkdirecve.ICESJournalofMarineScience.70(6),1055‐1064.
Galloway,T.S.(2015).Micro‐andnano‐plascsandhumanhealth.InMarineanthropogeniclitter
(pp.343‐366).SpringerInternaonalPublishing.
Galloway,T.S.,Cole,M.&Lewis,C.(2017).Interaconsofmicroplascdebristhroughoutthe
marineecosystem.NatureEcology&Evolution.1,0116.
Garrido S., Cruz, J., Santo, M. & Saiz, E. (2013). Effects of temperature, food type and food
concentraon on the grazing of the calanoid copepod Centropages chierchiae. Journal of
PlanktonResearch.35(4),843–854.
Gerritsen, J. (1984). Size efficiency reconsidered: a general foraging model for free‐swimming
aquacanimals.TheAmericanNaturalist.123,450‐467.
Gerritsen, J. & Strickler, J. R. (1977). Encounter probabilies and community structure in
zooplankton: a mathemacal model. Journal of the Fisheries Research Board of Canada. 34,
73‐82.
GESAMP‐JointGroupofExpertsontheScienficAspectsofMarineEnvironmentalProtecon
(2016).Sources,fateandeffectsofmicroplasticsinthemarineenvironment:Part2ofaglobal
assessment.ReportNo.93.Editors:P.J.Kershaw&C.M.Rochman.URL:www.gesamp.org.
Gewert,B.,Ogonowski,M.,Barth,A.&MacLeod,M.(2017).Abundanceandcomposionofnear
surfacemicroplascsandplascdebrisintheStockholmArchipelago,BalcSea.Marine
PollutionBulletin.120,1‐2.
Graham,E.R.&Thompson,J.T.(2009).Deposit‐andsuspension‐feedingseacucumbers
(Echinodermata)ingestplascfragments.JournalofExperimentalMarineBiologyandEcology.
368(1),22‐29.
Green, S., Visser, A.W., Titelman, J. & Kiørboe, T. (2003). Escape responses of copepod nauplii in
theflowfieldofthebluemussel,Mytilusedulis.MarineBiology.142(4),727‐733
Goldstein, M.C. & Goodwin, D.S. (2013). Gooseneck barnacles (Lepas spp.) ingest microplasc
debrisintheNorthPacificSubtropicalGyre.PeerJ.1,p.e184.
Goldstein, M.C., Titmus, A.J. & Ford, M. (2013). Scales of spaal heterogeneity of plasc marine
debrisintheNortheastPacificOcean.PLoSOne.10.1371/journal.pone.0080020.
Gorokhova, E. (2015). Screening for microplasc parcles in plankton samples: how to integrate
marine lier assessment into exisng monitoring programs? Marine Pollution Bulletin. 99(1‐2),
271–275.
Green, D.S. (2016). Effects of microplascs on European flat oysters, Ostrea edulis and their
associatedbenthiccommunies.EnvironmentalPollution.216,95‐103.
Green, D.S., Boots, B., Sigwart, J., Jiang, S. & Rocha, C. (2016). Effects of convenonal and
biodegradable microplascs on a marine ecosystem engineer (Arenicola marina) and sediment
nutrientcycling.EnvironmentalPollution.208,426‐434.
Green, S., Visser, A.W., Titelman, J. & Kiørboe, T. (2003). Escape responses of copepod nauplii in
theflowfieldofthebluemussel,Mytilusedulis.MarineBiology.142(4),727‐733.
Gutow, L., Eckerlebe, A., Gimenez, L. & Saborowski, R. (2015). Experimental evaluaon of
seaweeds as vector for microplascs into marine food webs. Environmental Science &
Technology.50,915–923.
Hammer, S., Nager, R.G., Johnson, P.C.D., Furness, R.W. & Provencher, J.F. (2016). Plasc debris in
great skua (Stercorarius skua) pellets corresponds to seabird prey species. Marine Pollution
Bulletin.103,206‐210.
Hara,T.J.(1975).OlfaconinfishProgressinNeurobiology.5(4),271‐335.
Harrison, J.P., Schratzberg, M., Sapp, M. & Osborn, A.M. (2014). Rapid bacterial colonizaon of
low‐density polyethylene microplascs in coastal sediment microcosms. BMC Microbiology.
14(1),232.
Hidalgo‐Ruz, V., Gutow, L., Thompson, R.C. & Thiel, M. (2012) Microplascs in the marine
environment: a review of the methods used for idenficaon and quanficaon.
EnvironmentalScience&Technology.46,3060‐307.
Holling, C.S. (1959). The components of predaon as revealed by a study of small‐mammal
predaonoftheEuropeanpinesawfly.TheCanadianEntomologist.91,293‐320.
Hüffer, T., Praetorius, A., Wagner, S., von der Kammer, F. & Hofmann, T. (2017). Microplasc
exposure assessment in aquac environments: Learning from similaries and differences to
engineerednanoparcles.EnvironmentalScience&Technology.51(5),2499–2507
Huntley, M.E., Barthel, K.G. & Star, J.L. (1983). Parcle rejecon by Calanus pacificus:
discriminaonbetweensimilarlysizedparcles.MarineBiology.74,151‐160.
Kaiser, D., Kowalski, N. & Waniek, J.J. (in press). Effects of biofouling on the sinking behavior of
microplascs.EnvironmentalResearchLetters.
Kautsky, L. & Kautsky, N. (2000). Balc Sea, including Bothnian Sea and Bothnian Bay. In:
Sheppard, C.R. C. (ed) Seas at the millennium: an environmental evaluaon. Elsevier Science
Ltd.Chapter8,p1–14.
Koehl M.A.R. & Sckler J.R. (1981). Copepod feeding currents: Food capture at low Reynolds
number.Limnology&Oceanography.26,1062‐1073.
Koelmans, A.A., Bakir, A., Burton, G.A. & Janssen, C.R. (2016). Microplasc as a vector for
chemicals in the aquac environment: crical review and model‐supported reinterpretaon of
empiricalstudies.EnvironmentalScience&Technology.50(7),3315‐3326.
Kiørboe, T., Møhlenberg, F. & Nicolajsen, H. (1982) Ingeson rate and gut clearance in the
planktonic copepod Centropages hamatus (Liljeborg) in relaon to food concentraon and
temperature.Ophelia.21,181‐194.
Kooi, M., Van Nes, E.H., Scheffer, M. & Koelmans, A.A. (2017). Ups and downs in the ocean: Effects
of biofouling on the vercal transport of microplascs. Environmental Science & Technology.
51(14),7963–7971doi:10.1021/acs.est.6b04702
Krümmel, E., Macdonald, RW., Kimpe, L.E., Gregory‐Eaves, I., Demers, M., Smol, J.P., Finney, B. &
Blais,J.M(2003).Deliveryofpollutantsbyspawningsalmon.Nature.425,255‐256
Laist, D. W. (1997). Impacts of marine debris: entanglement of marine life in marine debris
including a comprehensive list of species with entanglement and ingeson records. In Marine
Debris(pp.99‐139).SpringerNewYork.
Law, K.L., Morét‐Ferguson, S., Maximenko, N.A.., Proskurowski, G., Peacock, E.E.., Hafner, J. &
Reddy, C.M. (2010). Plasc Accumulaon in the North Atlanc Subtropical Gyre. Science. 329,
1185‐1188
Lee, K.W., Shim, W.J., Kwon, O.Y. & Kang, J.H. (2013). Size‐dependent effects of micro polystyrene
parcles in the marine copepod Tigriopus japonicus. Environmental Science & Technology. 47,
11278‐1183.
Ling, S.D., Sinclair, M., Levi, C.J., Reeves, S.E. & Edgar, G.J. (2017). Ubiquity of microplascs in
coastalseafloorsediments.MarinePollutionBulletin.121(1‐2),104‐110.
Lobelle, D. & Cunliffe, M. (2011). Early microbial biofilm formaon on marine plasc debris.
MarinePollutionBulletin.62(1),197‐200.
Long, M., Moriceau, B., Gallinari, M., Lambert, C., Huvet, A., Raffray, J. & Soudant, P. (2015).
Interacons between microplascs and phytoplankton aggregates: impact on their respecve
fates.MarineChemistry.175,39‐46.
Lusher, A.L., McHugh, M. & Thompson, R.C. (2013). Occurrence of microplascs in the
gastrointesnal tract of pelagic and demersal fish from the English Channel. Marine Pollution
Bulletin.67(1‐2),94‐99.
Lusher, A.L., Hernandez‐Milian, G., O'Brien, J., Berrow, S., O'Connor, I. & Officer, R. (2015).
Microplasc and macroplasc ingeson by a deep diving, oceanic cetacean: The True's beaked
whaleMesoplodonmirus.EnvironmentalPollution.199,185‐191.
Lusher, A.L.., Tirelli, V., O’Connor, I. & Officer, R. (2015). Microplascs in Arcc polar waters: the
first reported values of parcles in surface and sub‐surface samples. Scientific Reports. 5,
14947,srep14947.
Lusher, A.L., O’Donnell, C., Officer, R. & O’Connor, I. (2016). Microplasc interacons with North
Atlancmesopelagicfish.ICESJournalofMarineScience.73(4),1214‐1225.
Lusher, A.L., Welden, N.A., Sobral, P. & Cole, M. (2017). Sampling, isolang and idenfying
microplascsingestedbyfishandinvertebrates.AnalyticalMethods.9,1346‐1360.
Mathalon, A. & Hill, P. (2014). Microplasc fibers in the interdal ecosystem surrounding Halifax
Harbor,NovaScoa.MarinePollutionBulletin.81(1),69‐79.
Mato, Y., Isobe. T., Takada, H., Kanehiro, H., Ohtake, C. & Kaminuma, T. (2001). Plasc resin pellets
as a transport medium for toxic chemicals in the marine environment. Marine Pollution
Bulletin.35(2),318‐324
Miller, M.E., Kroon, F.J. & Mo, C.A. (2017). Recovering microplascs from marine samples: A
review of current pracces. Marine Pollution Bulletin. 123(1–2), 6‐18.
doi.org/10.1016/j.marpolbul.2017.08.058
Moore, S.L., Leecaster, M.K. & Weisberg, S.B. (2001) A comparison of plasc and plankton in the
northPacificcentralgyre.MarinePollutionBulletin.42,1297‐1300.
Mu, H., Ewald, G., Nilsson, E., Sundin, P. & Wese´n, C. (2004). Fate of chlorinated fay acids in
migrang sockeye salmon and their transfer to arcc grayling. Environmental Science &
Technology.38,5548‐5554.
Munari, C., Infanni, V., Scoponi, M., Rastelli, E., Corinaldesi, C. & Mistri, M. (2017). Microplascs
in the sediments of Terra Nova Bay (Ross Sea, Antarcca). Marine Pollution Bulletin. 122,
161–165.
Murray, P.R. & Cowie P.R. (2011). Plasc contaminaon in the decapod crustacean Nephrops
norvegicus(Linnaeus,1758).MarinePollutionBulletin.62,1207‐1217
NOAA ‐ Naonal Oceanic and Atmospheric Administraon Marine Debris Program (2014). Report
on the entanglement of marine species in marine debris with an emphasis on species in the
UnitedStates.SilverSpring,MD.pp.28
Nelms, S.E., Duncan, E.M., Broderick, A.C., Galloway, T.S., Godfrey, M.H., Hamann, M., Lindeque,
P.K. & Godley, B.J. (2015). Plasc and marine turtles: a review and call for research. ICES Journal
ofMarineScience:JournalduConseil.73(2),165‐181.
Nygaard, K., Borsheim, K.Y. & Thingstad, T.F. (1988). Grazing rates on bacteria by marine
heterotrophic microflagellates compared to uptake rates of bacterial‐sized monodisperse
fluorescentlatexbeads.MarineEcologyProgressSeries.44,159‐165.
Näkki, P., Setälä, O. & Lehniemi, M. (2017). Bioturbaon transports secondary microplascs to
deeper layers in so marine sediments of the northern Balc Sea. Marine Pollution Bulletin.
15;119(1):255‐261.doi:10.1016/j.marpolbul.2017.03.065.
Oberbeckmann, S., Loeder, M.G.J., Gerdts, G. & Osborn, M. (2014). Spaal and seasonal variaon
in diversity and structure of microbial biofilms on marine plascs in Northern European waters.
FEMSMicrobiologyEcology.90,478–492.
Ogonowski, M., Schür, C., Jarsén, Å. & Gorokhova, E. (2016). The effects of natural and
anthropogenic microparcles on individual fitness in Daphnia magna. PLoS ONE. 11(5),
e0155063.
Ogonowski, M., Wenman, D. & Gorokhova, E. (2017). Ingested microplasc is not correlated to
HOC concentraons in Balc Sea herring. 15th International Conference on Environmental
ScienceandTechnology.Rhodes,Greece,31Augustto2September2017.
Phuong, N.N., Zalouk‐Vergnoux, A., Poirier, L., Kamari, A., Châtel, A., Mouneyrac, C. & Lagarde, F.
(2016). Is there any consistency between the microplascs found in the field and those used in
laboratoryexperiments?EnvironmentalPollution.211,111‐123.
Railo, S. (2017). Microlier in Mytilus trossulus and its environment in the Northern Balc Sea:
Wastewateraspointsourcepolluon.MScthesis:UniversityofHelsinki,Finland.
Rescigno, M., Urbano, M., Valzasina, B., Francolini, M., Roa, G., Bonasio, R.. &
Ricciardi‐Castagnoli, P. (2001). Dendric cells express ght juncon proteins and penetrate gut
epithelialmonolayerstosamplebacteria.NatureImmunology.2(4).
Riisgård, H.U. and Larsen, P.S. (2010). Parcle capture mechanisms in suspension‐feeding
invertebrates.MarineEcologyProgressSeries,418:255‐293.doi.org/10.3354/meps08755.
Rochman, C.M., Tahir, A., Williams, S.L., Baxa, D.V., Lam, R., Miller, J.T., Teh, F., Werorilangi, S. &
Teh, S.J. (2015). Anthropogenic debris in seafood: Plasc debris and fibers from texles in fish
andbivalvessoldforhumanconsumpon.ScientificReports.5,14340.
Rummel, C.D., Jahnke, A., Gorokhova, E., Kühnel, D. & Schmi‐Jansen, M. (2017). The impacts of
biofilm formaon on the fate and potenal effects of microplasc in the aquac environment.
EnvironmentalScience&TechnologyLetters,4(7)258–267DOI:10.1021/acs.estle.7b00164
Schuyler, Q., Hardesty, B.D., Wilcox, C. & Townsend, K. (2012). To eat or not to eat? Debris
selecvitybymarineturtles.PLoSONE.7(7),e40884.
Setälä, O., Sopanen, S., Auo, R. & Erler, K. (2009): Grazing and prey selecon of the calanoid
copepods Eurytemora affinis and Acartia bifilosa feeding on plankton assemblages
containingDinophysisspp.BorealEnvironmentResearch.14,837‐849.
Setälä, O., Fleming‐Lehnen, V. & Lehniemi, M. (2014). Ingeson and transfer of microplascs in
theplanktonicfoodweb.EnvironmentalPollution.185:77‐83.
Setälä, O., Norkko, J., & Lehniemi, M. (2016). Feeding type affects microplasc ingeson in a
coastalinvertebratecommunity.Marinepollutionbulletin,102(1),95‐101.
Setälä, O., Magnusson, K., Lehniemi, M., & Norén, F. (2016). Distribuon and abundance of
surface water microlier in the Balc Sea: A comparison of two sampling methods. Marine
pollutionbulletin,110(1)177‐183.
Sherman, P. & Van Sebille, E. (2016). Modeling marine surface microplasc transport to assess
opmalremovallocaons.EnvironmentalResearchLetters,.11(1),014006.
Sileo, L., Sievert, P. R., Samuel, M. D., & Fefer, S. I. (1990). Prevalence and characteriscs of plasc
ingested by Hawaiian seabirds. In Proceedings of the Second International Conference on
MarineDebris(665‐681).NOAATechnicalMemoHonolulu.
Solomon, M.E. (1949). The natural control of animal populaons. Journal of Animal Ecology. 18,
1‐35
Staresinic, N., Farrington, J., Gagosian, R.B., Clifford, C.H. & Hulburt, E.M. (1983). Downward
transport of parculate maer in the Peru coastal upwelling: Role of the anchoveta, Engraulis
ringens. In: Suess, E. & Theide, J. (Eds.) Coastal Upwelling: Its Sediment Record. Part A.
Responses of the Sedimentary Regime to Present Coastal Upwelling. Plenum, New York, pp.
225–240.
Steer, M., Cole, M., Thompson, R.C. & Lindeque, P.K. (2017). Microplasc ingeson in fish larvae in
thewesternEnglishChannel.EnvironmentalPollution.226,250‐259.
Sun, X., Li, Q., Zhu, M., Liang, J., Zheng, S. & Zhao, Y. (2017). Ingeson of microplascs by natural
zooplankton groups in the northern South China Sea. Marine Pollution Bulletin. 115(1‐2),
217‐224.
Sussarellu, R., Suquet, M., Thomas, Y., Lambert, C., Fabioux, C., Pernet, M. E. J. & Huvet, A. (2016).
Oyster reproducon is affected by exposure to polystyrene microplascs. Proceedings of the
NationalAcademyofSciencesoftheUnitedStatesofAmerica.113(9),2430–2435.
Syberg, K., Khan, F.R., Selck, H., Palmqvist, A., Banta, G.T., Daley, J., Sano, L. & Duhaime, M.B.
(2015). Microplascs: addressing ecological risk through lessons learned. Environmental
Toxicology&Chemistry.34(5),945‐953.
Taylor, M.L., Gwinne, C., Robinson, L.F. & Woodall, L.C. (2016). Plasc microfibre ingeson by
deep‐seaorganisms.ScientificReports.6,33997.
Tiselius, P., Jonsson, P. R. & Verity, P. G. (1993). A model evaluaon of the impact of food
patchiness on foraging strategy and predaon risk in zooplankton. Bulletin of Marine Science.
53,247‐264.
Tourinho, P.S., Ivar do Sul, J.A. & Fillmann, G. (2010). Is marine debris ingeson sll a problem for
thecoastalmarinebiotaofsouthernBrazil?MarinePollutionBulletin.60(3),396‐401.
Turner, J.T. (2002). Zooplankton fecal pellets, marine snow and sinking phytoplankton blooms.
AquaticMicrobialEcology.27,57‐102
Turner, J.T. (2015). Zooplankton fecal pellets, marine snow, phytodetritus and the ocean’s
biologicalpump.ProgressinOceanography.130,205‐248.
Van Franeker, J.A., Blaize, C., Danielsen, J., Fairclough, K., Gollan, J., Guse, N., Hansen, P.L.,
Heubeck, M., Jensen, J.K., Le Guillou, G. & Olsen, B. (2011). Monitoring plasc ingeson by the
northern fulmar Fulmarus glacialis in the North Sea. Environmental Pollution. 159(10),
2609‐2615.
Van Franeker, J.A. & Law, K.L. (2015). Seabirds, gyres and global trends in plasc polluon.
EnvironmentalPollution.203,89‐96.
VanSebille,E.,Wilcox,C.,Lebreton,L.,Maximenko,N.,Hardesty,B.D.,VanFraneker,J.A.,Eriksen,
M.,Siegel,D.,Galgani,F.&Law,K.L.(2015).Aglobalinventoryofsmallfloangplascdebris.
EnvironmentalResearchLetters.10(12),124006.
Vandermeersch, G., Van Cauwenberghe, L., Janssen, C. R., Marques, A., Granby, K., Fait, G. &
Devriese, L. (2015). A crical view on microplasc quanficaon in aquac organisms.
EnvironmentalResearch.143,46‐55.
Volkenborn, N., Hedtkamp, S.I.C. Van Beusekom, J.E.E. & Reise, K. (2007). Effects of bioturbaon
and bioirrigaon by lugworms (Arenicola marina) on physical and chemical sediment
properes and implicaons for interdal habitat succession. Estuarine and Coastal Shelf
Science.74,331‐343.
von Moos, N., Burkhardt‐Holm, P. & Köhler, A. (2012). Uptake and effects of microplascs on cells
and ssue of the blue mussel Mytilus edulis L. aer an experimental exposure. Environmental
Science&Technology.46(20),11327‐11335.
Waller, C.L., Griffiths, H.J., Waluda, C.M., Thorpe, S.E., Loaiza, I., Moreno, B., Pacherres, C.O. &
Hughes, K.A. (2017). Microplascs in the Antarcc marine system: An emerging area of
research.ScienceofTheTotalEnvironment.598,220‐227.
Ward, J.E. & Koch, D.J. (2009). Marine aggregates facilitate ingeson of nanoparcles by
suspension‐feedingbivalves.MarineEnvironmentalResearch.68,137‐142.
Wa, A.J., Lewis, C., Goodhead, R.M., Becke, S.J., Moger, J., Tyler, C.R. & Galloway, T.S. (2014).
Uptake and retenon of microplascs by the shore crab Carcinus maenas. Environmental
Science&Technology.48(15),8823‐8830.
Woodall, L.C., Sanchez‐Vidal, A., Canals, M., Paterson, G.L.J., Coppock, R., Sleight, V., Calafat, A.,
Rogers, A.D., Narayanaswamy, B.E. & Thompson, R.C. (2014). The deep sea is a major sink for
microplascdebris.RoyalSocietyOpenScience,1(4),140317.DOI:10.1098/rsos.140317
Wright, S.L., Thompson, R.C. & Galloway T.S. (2013a). The physical impacts of microplascs on
marineorganisms:areview.EnvironmentalPollution.178,483‐492.
Wright, S.L., Rowe, D., Thompson, R.C. & Galloway, T.S. (2013b). Microplasc ingeson decreases
energyreservesinmarineworms.CurrentBiology.23(23),1031‐1033.
Ye, S. & Andrady, A.L. (1991). Fouling of floang plasc debris under Biscayne Bay exposure
condions.MarinePollutionBulletin.22,608–613.
Zeler, E. R., Mincer, T. J. & Amaral‐Zeler, L. A. (2013). Life in the “plassphere”: microbial
communiesonplascmarinedebris.Environmentalscience&technology,47(13),7137‐7146.