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  4. Tracing shifts of oceanic fronts using the cryptic diversity of the planktonic foraminifera Globorotalia inflata
 
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Tracing shifts of oceanic fronts using the cryptic diversity of the planktonic foraminifera Globorotalia inflata

Journal
Paleoceanography
Journal Volume
31
Journal Issue
9
Pages
1193-1205
Date Issued
2016
Author(s)
Morard R
Reinelt M
Chiessi C.M
JEROEN GROENEVELD  
Kucera M.
DOI
10.1002/2016PA002977
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84987978102&doi=10.1002%2f2016PA002977&partnerID=40&md5=6f219cc7574920e12f5fec29a21de3e7
https://scholars.lib.ntu.edu.tw/handle/123456789/624764
Abstract
The use of planktonic foraminifera in paleoceanographic studies relies on the assumption that morphospecies represent biological species with ecological preferences that are stable through time and space. However, genetic surveys unveiled a considerable level of diversity in most morphospecies of planktonic foraminifera. This diversity is significant for paleoceanographic applications because cryptic species were shown to display distinct ecological preferences that could potentially help refine paleoceanographic proxies. Subtle morphological differences between cryptic species of planktonic foraminifera have been reported, but so far, their applicability within paleoceanographic studies remains largely unexplored. Here we show how information on genetic diversity can be transferred to paleoceanography using Globorotalia inflata as a case study. The two cryptic species of G. inflata are separated by the Brazil-Malvinas Confluence (BMC), a major oceanographic feature in the South Atlantic. Based on this observation, we developed a morphological model of cryptic species detection in core top material. The application of the cryptic species detection model to Holocene samples implies latitudinal oscillations in the position of the confluence that are largely consistent with reconstructions obtained from stable isotope data. We show that the occurrence of cryptic species in G. inflata can be detected in the fossil record and used to trace the migration of the BMC. Since a similar degree of morphological separation as in G. inflata has been reported from other species of planktonic foraminifera, the approach presented in this study can potentially yield a wealth of new paleoceanographical proxies. ©2016. American Geophysical Union. All Rights Reserved.
Subjects
Brazil-Malvinas Confluence; cryptic diversity; morphometry
Other Subjects
fossil record; genetic variation; Holocene; morphology; morphometry; oceanic front; paleoceanography; planktonic foraminifera; reconstruction; species diversity; stable isotope; Atlantic Ocean; Atlantic Ocean (South); Brazil-Malvinas Confluence; Foraminifera; Globorotalia inflata
Type
journal article

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