Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...

Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflowing Atlantic water from Fram Strait, Yermak Plateau, northern Barents Sea continental slope as far as the Laptev Sea, have been analyzed for species richness and diversity. Samples were wet sieved af...

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Main Authors: Wollenburg, Jutta Erika, Mackensen, Andreas, Kuhnt, Wolfgang
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.527976
https://doi.pangaea.de/10.1594/PANGAEA.527976
id ftdatacite:10.1594/pangaea.527976
record_format openpolar
spelling ftdatacite:10.1594/pangaea.527976 2024-09-15T17:53:56+00:00 Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ... Wollenburg, Jutta Erika Mackensen, Andreas Kuhnt, Wolfgang 2007 application/zip https://dx.doi.org/10.1594/pangaea.527976 https://doi.pangaea.de/10.1594/PANGAEA.527976 en eng PANGAEA https://dx.doi.org/10.1016/j.palaeo.2007.05.007 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type Kasten corer ARK-III/3 ARK-VIII/3 ARK-IX/4 ARK-XIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.52797610.1016/j.palaeo.2007.05.007 2024-07-03T13:10:16Z Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflowing Atlantic water from Fram Strait, Yermak Plateau, northern Barents Sea continental slope as far as the Laptev Sea, have been analyzed for species richness and diversity. Samples were wet sieved after freeze-drying using a 63-µm sieve. Where possible at least 300 specimens were counted from the size fraction >63 µm, however, samples from deglacial periods are often affected by carbonate dissolution. In such samples foraminiferal numbers are low. Samples containing less than 40 specimens were excluded from statistical analyses. Because we are aware that specimen numbers <100 specimen are still critical for H analyses, core sections containing less than 100 specimens are highlighted in the figures. Here, we will characterize biodiversity trends by the two most widely used biodiversity measurements, the information function H (Buzas and Gibson, 1969) with its decomposition equation ln(S) and ln(E) (Buzas ... : Supplement to: Wollenburg, Jutta Erika; Mackensen, Andreas; Kuhnt, Wolfgang (2007): Benthic foraminiferal biodiversity response to a changing Arctic palaeoclimate in the last 24.000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 255(3-4), 195-222 ... Article in Journal/Newspaper Arctic Ocean Barents Sea Foraminifera* Fram Strait laptev Laptev Sea Yermak plateau DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
Kasten corer
ARK-III/3
ARK-VIII/3
ARK-IX/4
ARK-XIII/2
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
Kasten corer
ARK-III/3
ARK-VIII/3
ARK-IX/4
ARK-XIII/2
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Wollenburg, Jutta Erika
Mackensen, Andreas
Kuhnt, Wolfgang
Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...
topic_facet Gravity corer Kiel type
Kasten corer
ARK-III/3
ARK-VIII/3
ARK-IX/4
ARK-XIII/2
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflowing Atlantic water from Fram Strait, Yermak Plateau, northern Barents Sea continental slope as far as the Laptev Sea, have been analyzed for species richness and diversity. Samples were wet sieved after freeze-drying using a 63-µm sieve. Where possible at least 300 specimens were counted from the size fraction >63 µm, however, samples from deglacial periods are often affected by carbonate dissolution. In such samples foraminiferal numbers are low. Samples containing less than 40 specimens were excluded from statistical analyses. Because we are aware that specimen numbers <100 specimen are still critical for H analyses, core sections containing less than 100 specimens are highlighted in the figures. Here, we will characterize biodiversity trends by the two most widely used biodiversity measurements, the information function H (Buzas and Gibson, 1969) with its decomposition equation ln(S) and ln(E) (Buzas ... : Supplement to: Wollenburg, Jutta Erika; Mackensen, Andreas; Kuhnt, Wolfgang (2007): Benthic foraminiferal biodiversity response to a changing Arctic palaeoclimate in the last 24.000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 255(3-4), 195-222 ...
format Article in Journal/Newspaper
author Wollenburg, Jutta Erika
Mackensen, Andreas
Kuhnt, Wolfgang
author_facet Wollenburg, Jutta Erika
Mackensen, Andreas
Kuhnt, Wolfgang
author_sort Wollenburg, Jutta Erika
title Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...
title_short Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...
title_full Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...
title_fullStr Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...
title_full_unstemmed Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate ...
title_sort benthic foraminiferal biodiversity response to changing arctic palaeoclimate ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.527976
https://doi.pangaea.de/10.1594/PANGAEA.527976
genre Arctic Ocean
Barents Sea
Foraminifera*
Fram Strait
laptev
Laptev Sea
Yermak plateau
genre_facet Arctic Ocean
Barents Sea
Foraminifera*
Fram Strait
laptev
Laptev Sea
Yermak plateau
op_relation https://dx.doi.org/10.1016/j.palaeo.2007.05.007
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.52797610.1016/j.palaeo.2007.05.007
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