Crassatella baudeti (Coquand, 1862),来自Batna(阿尔及利亚东北部)的cenomanian:古生物地理学、古生态学和生物地层学

IF 1 4区 地球科学 Q4 PALEONTOLOGY
Riadh Aouissi , Sihem Salmi-Laouar , Izzet Hoşgör
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引用次数: 2

摘要

Batna地区(阿尔及利亚东北部)的下Cenomanian地层构成了大型无脊椎动物最丰富和最多样化的矿床,在标本和分类群方面主要以双壳类为主。其中,草苔科仅局限于塞诺曼阶地层的下层。它们的代表是单种博德蒂(Crassatella baudeti)。该物种很容易通过其扁平的船锚形状和相当强的近缘片层来区分,并且数量非常丰富。它存在于从Sharpeiceras schlueteri亚带到Cunningtoniceras inme带的各个层次。因此,该物种是下Cenomanian晚期和中Cenomanian早期的一个很好的标志。进行了精确的古生物学描述和环境讨论。因此,鲍德迪河可能是一个浅水环境的标志,具有寒冷但平静的水域,正常的盐度和中等柔软的基质。仅从特提斯的几个地方的塞诺曼尼亚记录,Cr. baudeti的独特存在反映了特定的热梯度和气候带。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Crassatella baudeti (Coquand, 1862) du Cénomanien de Batna (NE algérien) : paléobiogéographie, paléoécologie et biostratigraphie

The lower Cenomanian strata from the Batna region (NE Algeria) constitute the richest and most diversified deposits in terms of macro-invertebrates, mainly dominated by bivalves both in terms of specimens and taxa. Among them, Crassatellidae are restricted to the lower Cenomanian stratigraphical levels. They are represented by the single species Crassatella baudeti. The species is easily distinguished by its flattened boat anchor shape and quite strong commarginal lamellae, and is very abundant. It is present in levels ranging from Sharpeiceras schlueteri Subzone to Cunningtoniceras inerme Zone. The species is, therefore, a good marker of the last levels of the lower Cenomanian and the beginning of the midlle Cenomanian. A precise palaeontological description and an environmental discussion were conducted. Thus, Cr. baudeti would be indicative of a shallow environment, with cold but calm waters, normal salinity and moderately soft substrate. Recorded exclusively from the Cenomanian of a few Tethys localities, the exclusive presence of Cr. baudeti reflects a specific thermal gradient and climatic zonation.

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来源期刊
Annales de Paleontologie
Annales de Paleontologie 地学-古生物学
CiteScore
1.70
自引率
10.00%
发文量
8
审稿时长
>12 weeks
期刊介绍: Créées par Marcellin Boule en 1905, les Annales de Paléontologie publient 4 numéros par an traitant des fossiles animaux et végétaux, dans tous les domaines de la paléontologie incluant : -La Paléoanatomie- La Paléohistologie- La Morphologie fonctionnelle- La Systématique- L''Évolution- La Paléoécologie ... et toute les contributions susceptibles d''améliorer la compréhension des organismes et des environnements éteints.
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