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Bibliotheca Diatomologica, Band 26: Pinnularia: eine Monographie der europaischen Taxa

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... Esta variedade foi originalmente descrita por e caracterizada pelo intumescimento mediano das valvas e pelas extremidades arredondadas ou levemente dilatadas. Antes de propor a nova variedade, Krammer (1992a) interpretou os exemplares estudados como morfotipos (morfotipos 2 e 3) de P. acrosphaeria W. Smith var. acrosphaeria, os quais utilizou mais tarde para propor a atual var. ...
... A população estudada no presente estudo não apresentou variação morfológica. Krammer (1992aKrammer ( , 1992b incluiu vários morfotipos na circunscrição de P. mesolepta (Ehrenberg) W. Smith. A análise da espécie em Ehrenberg (1843), sua obra "princeps", mostrou que os representantes possuem valvas lineares, altamente onduladas e extremidades muito estreitas (rostradas, bem afiladas). ...
... O basiônimo de P. polyonca (Brébisson) Smith var. similis (Krammer) Krammer possui, em Krammer (1992a), a obra que contém a descrição original de P. mayeri, as seguintes dimensões: 52-82 µm compr., 8-10 µm larg. e 8-10 estrias alveoladas em 10 µm. ...
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Taxonomic survey of representatives of family Pinnulariaceae (Naviculales, Bacillariophyceae) in the Parque Estadual das Fontes do Ipiranga, São Paulo, Brazil. Two genera (Caloneis with 1 and Pinnularia with 12 species) and 20 taxa altogether, including 13 species and seven varieties that are not the typical of their respective species were identified. One variety, Pinnularia brauniana (Grunow) Mills var. sanctipaulensis Rocha, is described as new to science. Pinnularia brauniana (Grunow) Mills var. sanctipaulensis Rocha and P. subgibba Krammer var. lanceolata Gaiser & Johanser are the best geographically represented species in the Parque area occurring in 5 localities, whereas and Caloneis hyalina Hustedt, Pinnularia biceps Gregory var. biceps, P. grunowii Krammer, P. joculata (Manguin) Krammer, P. schoenfelderi Krammer, P. subanglica Krammer, P. tabellaria Ehrenberg and P. viridis (Nitzsch) Ehrenberg var. viridis are the least represented ones, been found in a single locality each.
... It should be kept in mind that ghost striae are often poorly distinguishable in light micrographs. For this reason, P. microgibba can be easily confused with certain diminutive species with narrow linear outlines and broad fascia, including the widespread, ubiquitous, and cosmopolitan P. sinistra [11,63]. However, P. microgibba has concave margins and a rhombic central area with ghost striae, whereas P. sinistra has a linear central area without markings (p. ...
... 265, Taf. 37, Figure 16 of [63]). Interestingly, a population of P. sinistra inhabiting the small oceanic island Île Amsterdam, situated in the southern part of the Indian Ocean (p. ...
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A new cyanobacterial species of Aliinostoc, A. vietnamicum sp. nov., is recorded in the tropical forest soil from the Cát Tiên National Park, Vietnam. The analysis is based on morphological characters, 16S rDNA phylogeny, ITS secondary structure, and fatty acid composition analysis. A. vietnamicum differed from the other species of the genus by the size and shape of vegetative cells, size of akinetes and heterocytes, and presence of granular polyphosphate inclusions in vegetative cells. The evolutionary distance matrix based on the 16S rRNA gene shared 96.2–98.2% similarities with other Aliinostoc sequences. The phylogeny inferred by Maximum Likelihood and Bayesian Inference placed A. vietnamicum in the Aliinostoc clade, within the Nostocaceae. For the first time, fatty acids composition analysis was obtained for a member of the genus Aliinostoc with cultivation time experiments. α‐linolenic (27.54–37.75%), palmitic (13.87–22.65%), and stearic (10.08–20.27%) acids were the dominant fatty acids when cultured during the exponential growth phase, as well as during stationary. This is the first finding of a strain with such a high content of stearic acid among cyanobacteria with Nostoc‐like morphology.
... Diatom slides were prepared from the surface sediments (0-1 cm) using standard procedures described, for example, by Battarbee et al. (2001). A minimum of 400 valves were identified with a phase-contrast light microscope at 10009 final magnification and using the nomenclature of Krammer andLange-Bertalot (1986-1991), Krammer (1992), Moser (1994), andHouk (2003). The taxonomic diversity of the diatom samples was calculated with Past software version 2.09 (Hammer et al., 2001) using individual rarefaction (Hurlbert, 1971). ...
... Diatom slides were prepared from the surface sediments (0-1 cm) using standard procedures described, for example, by Battarbee et al. (2001). A minimum of 400 valves were identified with a phase-contrast light microscope at 10009 final magnification and using the nomenclature of Krammer andLange-Bertalot (1986-1991), Krammer (1992), Moser (1994), andHouk (2003). The taxonomic diversity of the diatom samples was calculated with Past software version 2.09 (Hammer et al., 2001) using individual rarefaction (Hurlbert, 1971). ...
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The Iisalmi Route, a chain of lakes in central-eastern Finland, is more eutrophic than its surroundings. We used multivariate analyses to study the influence of selected environmental factors (water quality, basin characteristics, and subcatchment surficial geology) on the recent diatom assemblages across this steep local nutrient gradient. In addition to the spatial analysis of surface sediment diatom assemblages from 51 sampling sites (48 lakes), temporal changes in the total phosphorus (TP) concentrations of one Iisalmi Route lake (Lake Kirmanjärvi) were analyzed using weighted averaging partial least squares regression and 27 fossil diatom samples. Both TP and electrical conductivity (EC) showed statistically significant independent signals in the modern diatom data. The TP gradient was related to till grain size variation suggesting that geological factors affect the spatial TP variation directly or indirectly through differences in land use. Based on the temporal study, the direct effect of geology is most likely behind the steep nutrient gradient in the area because Lake Kirmanjärvi was found to be naturally eutrophic. EC, on the other hand, seems related to anthropogenic disturbance. Our study highlights the importance of taking the local geology into account when assessing past or present water quality or planning for lake management.
... Acaldera of the Golovnin Volcano; B -Golovnin cliff, composed of the Middle Pleistocene marine deposits and location of paleo-lake sequence; Clithology column with marker tephra and 14 C-dates; D -Photo of the paleo-lake sediments. Bertalot, 1986;1991a, b;Krammer, 1992). A minimum of 250 diatom frustules were counted. ...
Article
Despite considerable progress in understanding Late Pleistocene and Holocene palaeoenvironmental changes worldwide, there are still very few such data for the Far East, and Kuril islands, in particular. Here, the sea level rise during the Late Glacial–Holocene transition was accompanied by a loss of the land connectivity culminating into the development of isolated islands. The ecosystems evolution and importance of isolation for vegetation dynamics on islands are still insufficiently understood. We investigated a unique natural record of environmental change since 14 ka has been recently discovered in lake–mire complex on Kunashir Island. The sediments include 12 tephra layers from Kunashir and Hokkaido volcanoes. The lake level was highest during warmer and humid climate of the Allerød. Diatom assemblages indicated the higher lake level between 12 730–12 160 cal yr BP. The first half of Younger Dryas was characterized by heavy snowfalls. Cooling attributed to the Younger Dryas in the Southern Kurils was less distinct than on the continent. The pollen assemblages recorded changes in vegetation on the land bridge. At the end of the Pleistocene large areas were occupied by birch forests and shrub pine. The broadleaf species first appeared at the end of Allerød. Starting from the Pleistocene-Holocene transition and during the early Holocene, the role of conifers sharply increased. In the middle Holocene the proportion of broadleaf trees in forests increased. Coniferous forests became abundant during the Little Ice Age. Short-tern climatic fluctuations correlate well with regional pattern, particularly with fluctuations of the moisture supply.
... There is some row of small areolae on each alveolus in the quincunx pattern (Krammer, 2000). Generally, they have a groove and tongue raphe (Krammer, 1992a), however, they have changed in some large species which has made the outer fissure as the irregular course (complex raphe). ...
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The diatoms are widespread organisms that occurred in various environments like soil, marine, freshwater, and even in extreme conditions. Taleqhan River is one of the main tributaries of Sepid Roud, the second longest river in Iran with approximately 670 km length. During the sampling from eight stations in the Taleghan River and Dam, Pinnularia lundii var. linearis Krammer was identified as a new record for diatoms flora of Iran. Given the importance of Pinnularia genus as an indicator of pollution, it was discussed together with Pinnularia brebissonii (Kütz.) Krammer in this paper. This study was performed during November 2017 to October 2018 on the sediments monthly in the North of Iran. The most characteristic morphological features were the valve outline, density of striae, hexagonal shaped central area, non-deflected proxi-mal raphe endings and capitated apices. The most similar species to this taxon are P. suban-glica Petersen and Pinnularia biceps Gregory. They have deflected proximal raphe ending, unlike Pinnularia lundii var. linearis.
... The diatom slides were prepared and identified from the bottom and top sediment samples using standard procedures described by Battarbee et al. (2001). A minimum of 300 diatom valves were identified to the species level from each bottom sample with a phase-contrast light microscope (1000x final magnification) and using the taxonomic references of Krammer and Lange-Bertalot (1986, 1991a, Krammer (1992), Lange-Bertalot and Moser (1994), and Houk (2003). The top samples were identified otherwise similarly but with a minimum count of 400 (Tammelin et al., 2017) in order to improve the statistical reliability of the transfer function training set consisting of the top samples (Battarbee et al., 2001). ...
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Both natural and anthropogenic changes in boreal lakes have been studied utilizing paleolimnological methods, but the spatial variation in the natural conditions of lakes and its connection to geological factors has drawn less attention. Our aims were to examine the spatial distribution of naturally eutrophic lakes on the previously glaciated terrain of central-eastern Finland and the relationship between pre-human disturbance water quality and geological factors related to the basins and their catchments. Furthermore, we studied the pre- to post-human disturbance changes in the diatom assemblages and water quality of 48 lakes (51 sampling sites) across the pre-disturbance phosphorus gradient by using the top-bottom sampling approach and multivariate statistics. According to our results, naturally eutrophic boreal lakes are more common than previously thought, occurring on fine-grained and organic Quaternary landforms, including fine-grained till. Our study emphasizes the importance of the previously overlooked matter of till grain-size variation as a driver behind the spatial variation in the natural trophic states of boreal lakes. The location of a lake in the hydrologic landscape and basin morphology appear to be important factors as well. Shallow, naturally eutrophic lakes with short water residence times and high catchment area to lake area and volume ratios have been particularly sensitive to anthropogenic forcing. Our results indicate that cultural eutrophication is not the only water protection challenge for the relatively remote and dilute boreal lakes, but salinization and alkalinization are also serious threats that should be taken into account. Therefore, it is crucial to consider the notable variation in the natural conditions of boreal lakes in addition to mitigating the effects of anthropogenic forcing, such as nutrient loading, catchment erosion, salt pollution, and climate change, in order to achieve efficient water protection.
... Die Aufbereitung der Proben und die Bestimmung absoluter Valvenzahlen erfolgte nach den üblichen Standardverfahren (Battarbee, 1973;Battarbee & Kneen, 1982;Battarbee, 1986;Renberg, 1990 Die Bestimmungsbände der "Süßwasser -Flora Mitteleuropas" (Krammer & Lange-Bertalot, 1986 Krammer, 1989;Krammer, 1992;Lange-Bertalot, 1999), sowie Einzelveröffentlichungen __________________________________________________________________________________ (beispielsweise Kling & Håkannsson, 1988;Håkansson & Carter, 1990;Scheffler, 1994;Meyer & Håkansson, 1996;Hegewald & Hindáková, 1997) berücksichtigt. ...
... Diatom identifications were based on the works of Podzorski (1985), Krammer & Lange-Bertalot (1986, 1991a, b, 1997, Sala et al. (1993), Lange-Bertalot & Moser (1994, , , Witkowski et al. (1996), Metzeltin & Lange-Bertalot (1998), Lange-Bertalot & Genkal (1999, Reichardt (1999), Lange-Bertalot (2001), Krammer (1992Krammer ( , 1997Krammer ( , 2000Krammer ( , 2002 and Håkansson (1990Håkansson ( , 2002 for freshwater taxa and Witkowski et al. (2000) for marine forms. Diatoms were divided into groups according to their ecological requirements after Denys (1992), Hoffman (1994) and Van Dam et al. (1994). ...
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Relative abundance data of diatom (Bacillariophyceae) species were generated for sediment core SKPC-01B from the Skalafjord, Faeroe Islands. The record shows distinct temporal Changes in species composition. In the lowermost 65 cm of the 230 cm long core a species-rich freshwater diatom assemblage was found. Most of the taxa observed in this section are typical of oligotrophic to dystrophic lakes in northern Europe (Scandinavia, Iceland and Spitsbergen). Above this interval the diatom flora is dominated by marine taxa. The change from a freshwater to a marine flora is inferred to be caused by rising sea-level that took place about 7700-6400 years BP. Drastic changes in the diatom species composition within the transitional core section show that environmental change in the Skalafjord took place in several pulses. The first stage included strong inflow (possibly catastrophic) of marine waters. As a possible trigger of this phenomenon the tsunami released by the Storegga Slide is proposed. Before the final flooding by marine waters, freshwater conditions were re-eslablished within the Skalafjord. These results have important implications for the interpretation of the palaeogeographical development of the Eysturoy area. Hence, it is suggested that the Storegga Slide led to inflow of marine waters at a distinctly lower water level in the area of the Skalafjord than proposed in recent publications and that the inundation of the threshold in the fjord happened after the tsunami.
... Organic matter was oxidized from each sample using hydrogen peroxide and potassium dichromate before each sample was mounted and scanned at xlCKX) magnification under oil immersion and interference contrast. Nominally, 400 vaivae from each sample were identified to spedes or subspecies using Krammer & Lange-Bertalot (1986, 1988 and Krammer (1992) to provide data on percentage abundance. The few species not matching those described were given type labels for use in subsequent data analysis. ...
... Organic matter was oxidized from each sample using hydrogen peroxide and potassium dichromate before each sample was mounted and scanned at xlCKX) magnification under oil immersion and interference contrast. Nominally, 400 vaivae from each sample were identified to spedes or subspecies using Krammer & Lange-Bertalot (1986, 1988 and Krammer (1992) to provide data on percentage abundance. The few species not matching those described were given type labels for use in subsequent data analysis. ...
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1. Hydrobiological changes were assessed along an altirudinal transect of eighteen to twenty-three tributaries from 600 to 3750m in two adjacent river systems in east-central Nepal. The transect incorporated catchments under terraced agriculture at the lowest altitudes in the Likhu Khola, through streams in forest, alpine scrub and tundra at higher altitudes in Langtang. 2. Diatoms, bryophytes, macroinvertebrates and fish all showed pronounced altitudinal changes in assemblage composition as shown by TWINSPAN and DECORANA. A few taxa were restricted to streams at high altitude, but many more occurred only at lower altitudes where taxon richness increased substantially despite catchment disturbance by terraced agriculture. 3. Diatoms characteristic of lower altitude streams were mostly motile, epipelic or episammic Navicula and Nitzschia spp., which occur typically at greater electrolyte and nutrient concentrations. Those characteristic of higher and steeper sites included attached Fragilaria spp. and prostrate Achnanthes spp., tolerant of turbulent flow. 4. Cover by bryophytes varied within catchment type; high altitude springs supported dense mats, unlike streams fed by ice and glaciers. Taxa confined to low altitudes included those characteristic of humid subtropical conditions. 5. Invertebrate families occurring only at lower altitudes included a range of burrowers and pool dwellers. Numerically, filter feeding Hydropsychidae and Simuliidae dominated streams in terraced and forested catchments, whereas grazing baetid mayflies dominated higher altitude streams in scrub and tundra. 6. The combined density and biomass of at least six fish species in the Likhu Khola were 23–250 (per 100m−2), and 86–1282 g wet mass (per 100 m−2), respectively. No fish were found in Langtang streams, probably because torrential headwaters prevented colonization. 7. Our data confirm that altitudinal transitions in stream biota are pronounced in the Himalaya of Nepal, but are likely to reflect a wide array of potential influences.
... A minimum of 500 valves per sample was counted to the species or subspecies level. Taxonomy primarily followed Krammer and Lange-Bertalot (1986–1991), although several other references were important in making taxonomic determinations (Foged 1981, Germain 1981, Krammer 1992). Photographic images of all taxa from this study are available in Antoniades (2004). ...
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Diatom assemblages were analyzed from 64 lakes and ponds from Alert, Ellesmere Island and Mould Bay, Prince Patrick Island in the Canadian High Arctic Archipelago. Diverse water chemistry conditions and diatom communities were present in these sites. Small benthic taxa typically dominated diatom communities; however, assemblages were markedly different between Alert and Mould Bay sites in response to disparate water chemistry characteristics in the two regions. The most abundant taxa belonged to the genera Navicula, Cymbella, Achnanthes, Nitzschia, and Pinnularia. Canonical correspondence analysis indicated that pH, specific conductivity, dissolved organic carbon, and total phosphorus were the most important limnological variables in determining species composition. Diatom inference models were developed for pH, specific conductivity, and dissolved organic carbon using weighted averaging and weighted averaging partial least squares techniques; these had root mean square error of prediction/r2boot values of 0.40/0.77, 0.28/0.70, and 0.24/0.55, respectively. These models are applicable to sites with large ranges of taxonomic and limnological variation and will allow the reconstruction of past changes of climate-related limnological parameters from biostratigraphic records in future paleolimnological studies.
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We investigated the diatom ora of Fujiganaru Moor, an intermediate moor in Okayama Prefecture, Western Japan. It is a Sphagnum moor formed at the bottom of a valley at 220-240 m above sea level and is surrounded by a slightly sloped ridge. A field survey and sampling were taken place on 14 March 2016. The water was slightly acidic (pH 5.8-6.5) with low electrical conductivity (2.4-3.2 mS m-1). From 15 samples, 111 diatom taxa belonging to 32 genera were found, although 16 of them have not been identified at the species level. They are all listed and illustrated here. In terms of taxa richness, the dominant genus was Pinnularia, represented by 24 taxa, followed by Eunotia, with 17 taxa.
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The benthic diatoms collected during our recent research in athalassic habitats exemplify a high morphological variability within Chamaepinnularia krookiformis Lange-Bertalot et Krammer. The species has already been known from freshwater ecosystems as well as from brackish waters in different regions of Europe. This variability has been also confirmed by the analysis of the literature. However, this is the first time that the morphological variability of the species has been addressed. In order to revise C. krookiformis and describe a new species, which has been distinguished on the basis of our material, we compared it with the type material of Pinnularia krookiformis Krammer 1992 from the periodic saline pool in Nordrhein-Westfalen (Germany). This study deals with a morphological analysis based on a large populations of C. krookiformis from Pełczyska (Central Poland). Selected morphological features were analysed, i.e.: valve length and width, number of striae in 10 µm, apices width, constrictions width, apices/constrictions width ratio, central-area length, and valve/central area length ratio. The results of light (LM) and scanning (SEM) microscopy, supported by multidimensional scaling (MDS), allowed for the distinction of three different morphotypes. Two of them match Krammer concept of Pinnularia krookiformis from 1992, while the third, occurring in our samples in three sampling sites, is clearly different. Thus, we described a new species Chamaepinnularia plinskii sp. nov., by the following major features: the valves are linear, symmetric, with rounded, capitate apices, the axial area is narrow, expanding to a wide central area forming a fascia, distal raphe endings are hooked to the same side of the valve and striae slightly radiate in the middle and in the rounded apices, becoming parallel in constrictions, 20-26 in 10 µm. This species occurs in inland waters with a wide range of chloride concentration, from 1000 to 3500 mg.l-1.
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Langzeiteffekte von Umwelteinflüssen dokumentieren sich in den Ablagerungen von Ozeanen, Seen, Mooren, Grundwasser, in terrestrischen Ökosystemen, wie z. B. Böden, aber auch im Eis der Polarregionen. In der Paläolimnologie verwendet man physikalische, chemische und biologische Informationen aus dem Sediment, um die früheren Umweltbedingungen eines Sees zu rekonstruieren. In diesem Beitrag sollen die Möglichkeiten und die Probleme der Paläolimnologie an Hand von Seesedimenten dargestellt werden. Es werden verschiedene Untersuchungsmethoden an umweltrelevanten Parametern und neue Forschungsergebnisse diskutiert und die praktischen Anwendungsmöglichkeiten kritisch beleuchtet.
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The periphytic diatom flora of Nakaikemi Wetland, a peaty low moor located near the Sea of Japan in Fukui Prefecture, central Japan, was studied. This moor was inscribed as a registered wetland under the Ramsar Convention in 2012. We checked a total of 50 diatom samples collected from the surface of filamentous green algae, living/dead spermatophytes, and mud in the moor in May and November, 2008. The water ranged from slightly acidic to alkaline (pH 5.9–8.8), and electrical conductivity also varied greatly among sites (7–32 mS m-1). In all, 297 taxa belonging to 61 genera are listed and illustrated from these samples, although 36 taxa among them have not been identified to species. In terms of taxa richness, the dominant genus was Pinnularia, represented by 35 taxa, followed by Navicula (24 taxa), Nitzschia and Gomphonema (23 taxa each), and Sellaphora (21 taxa). Several brackish and/or marine diatoms occurred in the samples although the water was fresh. Navicula americana var. moesta Temp. et H.Perag. is raised to species level with its transfer to the genus Sellaphora, as S. moesta (Temp. et H.Perag.) Ohtsuka comb. nov.
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