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首页> 外文期刊>Journal of Paleontology >Taxonomy, ontogeny and paleoecology of two species of Harbinia TSAO, 1959 (Crustacea, Ostracoda) from the santana formation, lower cretaceous, Northeastern Brazil
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Taxonomy, ontogeny and paleoecology of two species of Harbinia TSAO, 1959 (Crustacea, Ostracoda) from the santana formation, lower cretaceous, Northeastern Brazil

机译:来自巴西东北下白垩统桑塔纳组的1959年哈尔滨TSAO两种物种(甲壳纲,Ostracoda)的分类学,本体论和古生态学

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The Araripe Basin is the most extensive interior basin in northeastern Brazil, comprising areas of Cear, Piauí and Pernambuco states. The Santana Formation, attributed to the Aptian?lower Albian age of the basin, is subdivided into two members, Crato and Romualdo, which bear an abundant fossil record of plant fragments, arthropods and vertebrates, especially 3D-preserved fishes. The present study focuses on the taxonomy, ontogeny and paleoecology of two ostracode species from the Romualdo Member and the top section of the Crato Member (Ipubi layers), Harbinia salitrensis (Krmmelbein and Weber, 1971) emend. and H. alta new species. The ontogenetic series for both species are illustrated, except for the A-8 instar; H. salitrensis is also redescribed. The present work is also the first to produce quantitative information about the paleoecology of the Santana Formation based on ostracode populations. The results obtained from analyses of the population age-structure of both species, in addition to dominance (Simpson) and diversity index (Shannon) values, corroborated previous data on the studied sequence. According to these results, the strata were deposited in a limnic, low-to-moderate energy environment with salinity levels varying from oligohaline to mesohaline. The new data indicate the possibility of these environments also being hypersaline.
机译:Araripe盆地是巴西东北部最广阔的内陆盆地,由Cear,Piauí和Pernambuco州组成。桑塔纳岩层归因于该盆地的阿普第安较低的阿尔比时代,它分为两个组成部分,克拉托(Crato)和罗曼杜(Romaualdo),它们具有丰富的植物碎片,节肢动物和脊椎动物化石记录,尤其是保存3D的鱼类。本研究的重点是来自Romualdo成员和Crato成员顶部(伊波西层)的两种Ostracode物种的分类学,本体论和古生态学(Harmania salitrensis)(Krmmelbein和Weber,1971)。和H. alta新物种。说明了两个物种的个体发育序列,除了A-8龄; salitrensis也被重新描述。本研究也是第一份基于Ostracode种群产生有关桑塔纳组古生态定量信息的信息。除优势度(Simpson)和多样性指数(Shannon)值外,对这两个物种的种群年龄结构进行分析的结果均证实了先前关于该序列的数据。根据这些结果,地层沉积在盐度从低盐度到中盐度不等的石灰岩,低至中度能量环境中。新数据表明这些环境也可能成为超盐度。

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