A review of the importance of the Caribbean region in Oligo-Miocene low latitude planktonic foraminiferal biostratigraphy and the implications for modern biogeochronological schemes
A review of the importance of the Caribbean region in Oligo-Miocene low latitude planktonic foraminiferal biostratigraphy and the implications for modern biogeochronological schemes
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加勒比地区在渐新世低纬度浮游有孔虫生物地层学中的重要性及其对现代生物地质年代学方案的影响
DOI：
10.1016/j.earscirev.2019.102968
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发表时间：
2020
影响因子：
12.1
通讯作者：
King D
中科院分区：
文献类型：
--
作者：
King D
浮游有孔虫因其体积小、分布范围小、在海洋沉积物中丰度高而被广泛应用于海洋生物地层学研究。世纪中期，加勒比地区首次充分认识到浮游有孔虫在生物地层学中的作用。该地区是低纬度生物地层学的后续发展的关键，仍然是现代生物年代学的基础。本研究对这些生物地层学方案中的渐新世-中新世组成部分进行了历史回顾，包括Cushman和Alfrethforth（1945）首次提出的方案以及随后的发展。Hans Bolli和Walter Blow的工作特别突出，因为他们对现代生物地层学产生了重大影响，包括这些作者最初认识到一些生物事件的生物地层学效用至今仍然适用。这些以加勒比海为中心的方案与Wade等人（2011年）的现代低纬度生物年代学相关联，这一综合强调了一些生物事件（例如TopParagloborotalia kugleri和TopCatapsydrax dissimilis）自最初被认识以来一直被应用。这反过来又允许这些生物事件的可识别性根据每个数据的一致性来推断。此外，重新评估了重点关注加勒比地区的六项研究的范围图，以确定是否有可能应用给定的生物事件，原作者只是没有认识到该物种的生物地层学效用或倾向于另一种生物事件。建议对Wade等人（2011年）进行一些修正，并建议今后优先考虑南极有孔虫年代学。最值得注意的是，重新引入BaseGlobigerinatella insuetaas作为一个主要的生物事件，由于该物种的历史生物地层学的重要性。这一事件现在定义了早中新世分区M3 b（Gt. insueta/Ct. dissimilisPRZ）将区M3划分成上部子区M3 b（BaseGt. insueta）和下亚区M3 a（BaseGlobigerinatellasp.）。最后，Wade等人（2011年）的中新世至近代时间尺度在最近更新磁性地层学之后重新校准（Kochhann等人，2016; Ogg等人，2016; Drury等人，2017; Beddow等人，2018）和旋回地层学（Wilkens等人，2017年）。对南极有孔虫年代学的总体影响是微小的，但我们的结果成为低纬度地区的建议生物地层框架。
Planktonic foraminifera are widely used in marine biostratigraphy thanks to their small size, limited stratigraphic range and abundance in oceanic sediments. The utility of planktonic foraminifera in biostratigraphy was first fully recognised within the Caribbean region during the middle of the 20th century. The area was critical for the subsequent development of the low latitude biostratigraphic schemes and remains fundamental for modern day biogeochronologies. This study presents a historical review of the Oligo-Miocene component of these biostratigraphic schemes, including the first proposed scheme of Cushman and Stainforth (1945) and the subsequent development. The work of Hans Bolli and Walter Blow is particularly highlighted due to their heavy influence on modern day biostratigraphy, including these authors initially recognising the biostratigraphic utility of a number of bioevents still applied today. These Caribbean-centric schemes are correlated to the modern-day low latitude biogeochronology of Wade et al. (2011), with this synthesis highlighting that a number of bioevents (e.g. TopParagloborotalia kugleriand TopCatapsydrax dissimilis) have been applied consistently since their initial recognition. This in turn allows the recognisability of these bioevents to be deduced based on how consistently applied each datum has been. In addition, the range charts of six studies focusing heavily on the Caribbean have been reassessed to determine whether there is potential to apply a given bioevent, and the original author merely did not recognise the biostratigraphic utility of the species or favoured another bioevent.In considering this historical review, a number of amendments to Wade et al. (2011) and future priorities to planktonic foraminifera biogeochronologies are suggested. Most notably, the re-introduction of BaseGlobigerinatella insuetaas a primary bioevent due to the historical biostratigraphic importance of this species. This event now defines early Miocene Subzone M3b (Gt. insueta/Ct. dissimilisPRZ) dividing Zone M3 into an upper Subzone M3b (BaseGt. insueta) and lower Subzone M3a (BaseGlobigerinatellasp.). Finally, the Miocene to Recent timescale of Wade et al. (2011) has been recalibrated following more recent updates to the magnetostratigraphy (Kochhann et al., 2016; Ogg et al., 2016; Drury et al., 2017; Beddow et al., 2018) and cyclostratigraphy (Wilkens et al., 2017). The overall effect on the planktonic foraminifera biogeochronology is minor but our results become the suggested biostratigraphic framework for the low latitudes.
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重访赤道大西洋塞阿拉隆起：ODP Leg 154 0 至 5 Ma 的同位素地层学
影响因子：
4.3
作者：
Wilkens;Westerhold;Gorgas
通讯作者：
Gorgas
影响因子：
3.7
作者：
Spezzaferri S;Kucera M;Pearson PN;Wade BS;Rappo S;Poole CR;Morard R;Stalder C
通讯作者：
Stalder C
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影响因子：
4.9
作者：
R. Poore;L. Tauxe;S. F. Percival;Labrecque;J. Wright;R. Petersen;N. P. Smith;C. Tucker;P. Hsu
通讯作者：
P. Hsu
二十世纪巴塞尔（瑞士）的微型古生物学：生命科学较小领域之一的兴衰
DOI：
10.1144/tms6.23
发表时间：
2013
期刊：
Bulletins of American Paleontology
影响因子：
--
作者：
L. Hottinger
通讯作者：
L. Hottinger
劳盆地和汤加地台第 135 段的中新世至更新世浮游有孔虫生物地层
影响因子：
1.3
作者：
G. Chaproniere;H. Nishi
通讯作者：
H. Nishi