Figura 3 - uploaded by Manuel Abad
Content may be subject to copyright.
a-d: Braquiópodos de la Formación Calcarenita de Niebla: Terebratula maugerii Boni. a: Vista dorsal (NIE-B-1-1); b: Vista lateral (NIE-B-1-1); c: Vista interna de una valva ventral (NIE-B-1-4); d: Vista interna de una valva dorsal (NIE-B-1-5). e-h: Braquiópodos de la Formación Arenas de Huelva: Maltaia pajaudi García Ramos. e: Vista dorsal (CP-B-1); f: Vista lateral (CP-B-1); g: Vista interna de una valva ventral (CP-B-10); h: Vista interna de una valva dorsal (CP-B-9). i-l: Braquiópodos de la Formación Arcillas de Gibraleón: Cryptopora sp. i: Vista dorsal (TRIG-B-1); j: Vista ventral (TRIG-B-1); k: Vista ventral (TRIG-B-2); l: Vista dorsal (TRIG-B-2). Escala a-i: 1 cm; i-l: 1 mm.
Source publication
This paper analyzes the first brachiopod record of three Neogene formations of the southwestern Guadalquivir Basin (Huelva province, SW Spain) with a wide cartographical distribution. Samples obtained in five sections of these formations have allowed to recognize three species belonging to the genera Terebratula, Maltaia and Cryptopora, the latter...
Similar publications
The Kerala Basin is only onshore opportunity to study Cenozoic palaeoclimate and palaeoenvironment of southwest India encompassing Neogene global events such as Mid Miocene Climate Optimum (MMCO) and even older times of Palaeogene. The global warming during ~17–15 Ma (MMCO), enhanced annual surface temperature 3–4° C higher than the present, is equ...
Phymatellid demosponges are common fossils in the Campanian deposits of central Europe. In Poland, the Campanian phymatellids were known mostly from the opoka facies of the Miechów Synclinorium (southern Poland), where they occur mainly in the characteristic horizons of siliceous nodules in the lower Campanian opoka succession. Similarly preserved...
The upper Miocene – lower Pliocene sedimentary succession of the Denizli Basin (SW Anatolia) displays a unique record of undisturbed stratigraphy and provides an excellent opportunity to study long-term palaeoecological changes. This paper documents the ostracod assemblages of two sections of the Neogene Kolankaya Formation, resulting in the follow...
In Morocco, diatomite sedimentation is mainly known in the Neogene basins of the North Eastern Rif. The most important deposits are located in the Boudinar basin and the Mellilia-Nador basin. This study is devoted to the enhancement of this natural geo-resource in the construction of the building. The objective of this work is on the one hand, the...
