A larger benthic foraminiferal zonation for the Eocene of the Caribbean and central American region

IF 1.5 4区 地球科学 Q2 GEOLOGY Carnets De Geologie Pub Date : 2022-07-01 DOI:10.2110/carnets.2022.2211
S. Mitchell, E. Robinson, E. Özcan, M. Jiang, Natalie Robinson
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引用次数: 3

Abstract

We have undertaken a study of the larger benthic foraminifera (LBF) of the Eocene of Jamaica that involved collecting free specimens and calibrating their occurrence against chronostratigraphy using calcareous nannofossils identified from sample splits or adjacent samples. The results have been plotted stratigraphically and allow a detailed zonation of the Eocene (14 zones) to be developed based largely on lepidocyclinids and similar forms. The zonation can be shown to be applicable to the Americas extending from northern South America, to Central America, the Caribbean and southern North America. The LBF biostratigraphy is based on the evolution of various groups. Three zones are recognized in the Ypresian, six zones in the Lutetian, three zones in the Bartonian, and two zones in the Priabonian. In order to classify the LBF we have revised the important groups used for the zonation scheme that occur in the Eocene and figure numerous examples. Our revision rearranges described genera into evolutionary, monophyletic clades to which we give the hierarchy of family and subfamily. We provide remarks on published taxa explaining how they are recognized and describe all the new taxa (two families, one subfamily, four genera and five species). The following families, genera and species are new: Butterliniana gen. nov., Helicosteginidae fam. nov., Helicostegina minor sp. nov., Helicostegina jamaicensis sp. nov., Helicostegina jeannemairae sp. nov., Pseudolepidinidae fam. nov., Orbitoininae subfam. nov., Planorbitoinella gen. nov., Polyorbitoinella gen. nov., Polyorbitoinella lilyfieldensis sp. nov., Orbitoina wrighti sp. nov., and Nephronummulites gen. nov.
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加勒比和中美洲地区始新世较大的底栖有孔虫带
我们对牙买加始新世的大型底栖有孔虫(LBF)进行了一项研究,包括收集免费标本,并使用从样本分离或邻近样本中鉴定的钙质纳米化石,根据年代地层学校准它们的发生。结果已被绘制成地层学图,并允许对始新世(14个带)进行详细的分带,主要基于鳞状环类和类似的形式。这一分区可以证明适用于从南美洲北部延伸到中美洲、加勒比和北美洲南部的美洲。LBF生物地层学是以各群的演化为基础的。伊波斯系有3个带,鲁特梯系有6个带,巴顿系有3个带,普里亚伯尼亚系有2个带。为了对LBF进行分类,我们修改了始新世用于分区方案的重要群,并列举了许多例子。我们的修订将描述的属重新排列为进化的单系分支,我们给出了科和亚科的层次结构。我们对已发表的分类群进行了注释,解释了它们是如何被识别的,并描述了所有新分类群(2科,1亚科,4属和5种)。以下科、属、种为新种:毛茛属、螺帽藻科;11月,小螺蛳虫,牙买加螺蛳虫,jeannemaaiae螺蛳虫,假绦虫科。11月,轨道轨道亚群。11月,Planorbitoinella gen. nov., Polyorbitoinella gen. nov., Polyorbitoinella lilfieldensis sp. nov., Orbitoina wright sp.,和Nephronummulites gen. nov.。
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来源期刊
Carnets De Geologie
Carnets De Geologie Earth and Planetary Sciences-Geology
CiteScore
2.90
自引率
14.30%
发文量
21
审稿时长
>12 weeks
期刊介绍: Information not localized
期刊最新文献
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