(Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...

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 pl...

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Main Authors: Morard, Raphael, Reinelt, Melanie, Chiessi, Cristiano Mazur, Groeneveld, Jeroen, Kucera, Michal
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2016
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.864220
https://doi.pangaea.de/10.1594/PANGAEA.864220
id ftdatacite:10.1594/pangaea.864220
record_format openpolar
spelling ftdatacite:10.1594/pangaea.864220 2024-09-15T18:30:47+00:00 (Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ... Morard, Raphael Reinelt, Melanie Chiessi, Cristiano Mazur Groeneveld, Jeroen Kucera, Michal 2016 application/zip https://dx.doi.org/10.1594/pangaea.864220 https://doi.pangaea.de/10.1594/PANGAEA.864220 en eng PANGAEA https://dx.doi.org/10.1002/2016pa002977 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Center for Marine Environmental Sciences MARUM Geosciences, University of Bremen GeoB article Collection Supplementary Publication Series of Datasets 2016 ftdatacite https://doi.org/10.1594/pangaea.86422010.1002/2016pa002977 2024-08-01T11:01:20Z 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 ... : Supplement to: Morard, Raphael; Reinelt, Melanie; Chiessi, Cristiano Mazur; Groeneveld, Jeroen; Kucera, Michal (2016): Tracing shifts of oceanic fronts using the cryptic diversity of the planktonic foraminifera Globorotalia inflata. Paleoceanography, 31(9), 1193-1205 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Center for Marine Environmental Sciences MARUM
Geosciences, University of Bremen GeoB
spellingShingle Center for Marine Environmental Sciences MARUM
Geosciences, University of Bremen GeoB
Morard, Raphael
Reinelt, Melanie
Chiessi, Cristiano Mazur
Groeneveld, Jeroen
Kucera, Michal
(Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...
topic_facet Center for Marine Environmental Sciences MARUM
Geosciences, University of Bremen GeoB
description 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 ... : Supplement to: Morard, Raphael; Reinelt, Melanie; Chiessi, Cristiano Mazur; Groeneveld, Jeroen; Kucera, Michal (2016): Tracing shifts of oceanic fronts using the cryptic diversity of the planktonic foraminifera Globorotalia inflata. Paleoceanography, 31(9), 1193-1205 ...
format Article in Journal/Newspaper
author Morard, Raphael
Reinelt, Melanie
Chiessi, Cristiano Mazur
Groeneveld, Jeroen
Kucera, Michal
author_facet Morard, Raphael
Reinelt, Melanie
Chiessi, Cristiano Mazur
Groeneveld, Jeroen
Kucera, Michal
author_sort Morard, Raphael
title (Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...
title_short (Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...
title_full (Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...
title_fullStr (Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...
title_full_unstemmed (Supplementary Material 2) Landmark coordinates of the analyzed specimens with associated metadata ...
title_sort (supplementary material 2) landmark coordinates of the analyzed specimens with associated metadata ...
publisher PANGAEA
publishDate 2016
url https://dx.doi.org/10.1594/pangaea.864220
https://doi.pangaea.de/10.1594/PANGAEA.864220
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.1002/2016pa002977
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.86422010.1002/2016pa002977
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