Diatom abundance in surface sediments of the Southern Ocean

The quantitative analysis of diatom assemblages preserved in 52 samples from the Bellingshausen and the Amundsen Seas provides the first comprehensive view on the distribution of diatoms in surface sediments of the eastern and central Pacific sector of the Southern Ocean. On a latitudinal transect a...

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Bibliographic Details
Main Authors: Esper, Oliver, Gersonde, Rainer, Kadagies, Nicole
Format: Dataset
Language:English
Published: PANGAEA 2010
Subjects:
MUC
PLA
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.681699
https://doi.org/10.1594/PANGAEA.681699
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.681699
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Actinocyclus actinochilus
Actinocyclus curvatulus
Amundsen Sea
ANT-XI/3
ANT-XII/4
ANT-XVIII/5a
Asteromphalus hookeri
Asteromphalus hyalinus
Asteromphalus parvulus
AWI_Paleo
Azpeitia tabularis var. egregius
Azpeitia tabularis var. tabularis
Chaetoceros spp.
Counting
diatoms
DEPTH
sediment/rock
Diatoms indeterminata
Elevation of event
Eucampia antarctica
Event label
Fragilariopsis curta
Fragilariopsis cylindrus
Fragilariopsis doliolus
Fragilariopsis kerguelensis
Fragilariopsis obliquecostata
Fragilariopsis rhombica
Fragilariopsis ritscheri
Fragilariopsis separanda
Fragilariopsis sublinearis
Hemidiscus cuneiformis
Latitude of event
Longitude of event
MUC
MultiCorer
Nitzschia bicapitata
Nitzschia kolaczeckii
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
PLA
Plankton net
Polarstern
Porosira glacialis
PS2546-1
PS2547-2
PS2548-2
PS2550-2
PS2657-1
PS2659-2
PS2661-4
spellingShingle Actinocyclus actinochilus
Actinocyclus curvatulus
Amundsen Sea
ANT-XI/3
ANT-XII/4
ANT-XVIII/5a
Asteromphalus hookeri
Asteromphalus hyalinus
Asteromphalus parvulus
AWI_Paleo
Azpeitia tabularis var. egregius
Azpeitia tabularis var. tabularis
Chaetoceros spp.
Counting
diatoms
DEPTH
sediment/rock
Diatoms indeterminata
Elevation of event
Eucampia antarctica
Event label
Fragilariopsis curta
Fragilariopsis cylindrus
Fragilariopsis doliolus
Fragilariopsis kerguelensis
Fragilariopsis obliquecostata
Fragilariopsis rhombica
Fragilariopsis ritscheri
Fragilariopsis separanda
Fragilariopsis sublinearis
Hemidiscus cuneiformis
Latitude of event
Longitude of event
MUC
MultiCorer
Nitzschia bicapitata
Nitzschia kolaczeckii
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
PLA
Plankton net
Polarstern
Porosira glacialis
PS2546-1
PS2547-2
PS2548-2
PS2550-2
PS2657-1
PS2659-2
PS2661-4
Esper, Oliver
Gersonde, Rainer
Kadagies, Nicole
Diatom abundance in surface sediments of the Southern Ocean
topic_facet Actinocyclus actinochilus
Actinocyclus curvatulus
Amundsen Sea
ANT-XI/3
ANT-XII/4
ANT-XVIII/5a
Asteromphalus hookeri
Asteromphalus hyalinus
Asteromphalus parvulus
AWI_Paleo
Azpeitia tabularis var. egregius
Azpeitia tabularis var. tabularis
Chaetoceros spp.
Counting
diatoms
DEPTH
sediment/rock
Diatoms indeterminata
Elevation of event
Eucampia antarctica
Event label
Fragilariopsis curta
Fragilariopsis cylindrus
Fragilariopsis doliolus
Fragilariopsis kerguelensis
Fragilariopsis obliquecostata
Fragilariopsis rhombica
Fragilariopsis ritscheri
Fragilariopsis separanda
Fragilariopsis sublinearis
Hemidiscus cuneiformis
Latitude of event
Longitude of event
MUC
MultiCorer
Nitzschia bicapitata
Nitzschia kolaczeckii
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
PLA
Plankton net
Polarstern
Porosira glacialis
PS2546-1
PS2547-2
PS2548-2
PS2550-2
PS2657-1
PS2659-2
PS2661-4
description The quantitative analysis of diatom assemblages preserved in 52 samples from the Bellingshausen and the Amundsen Seas provides the first comprehensive view on the distribution of diatoms in surface sediments of the eastern and central Pacific sector of the Southern Ocean. On a latitudinal transect along 120°W, diatom valve accumulation rates (AR) reach maximum values (8–10 × 10**8 valves m**-2 yr**-1) in a zone extending over ca. 900 km between the Antarctic Polar Front and the maximum average winter sea ice extent and exceed those ARs obtained from an eastern transect along 90°W by one order of magnitude. Lowest diatom concentrations (1–3 × 10**6 valves g**-1) were encountered in sediments of the Sea Ice Zone, affected by winter and summer sea ice. The accumulation rate pattern of the most abundant diatom Fragilariopsis kerguelensis (> 50% abundance in 47 samples) mirrors the pattern of the total diatom valve AR and the biogenic silica (BSi) AR, making F. kerguelensis the major contributor to the BSi preserved at the sea floor. Relative abundances of diatom species and species groups were statistically compared with a selection of environmental variables, such as the mean summer sea surface temperature and salinity, mean annual surface nutrient concentration (nitrate, phosphate, silicon), mean annual water column stratification, mixed layer depth in summer, and mean summer and winter sea ice concentrations. Polynomial canonical redundancy analysis (RDA) revealed the biogeographic distribution of diatom species had the strongest relationship with summer sea surface temperature (SSST) out of the nine tested environmental variables. This relationship accounted for 69.6% of the total variance of the diatom distribution, with 29.7% explained by the first gradient (significantly correlated to SSST with r**2 = 0.941) and 15.6% explained by the second gradient (correlated to both summer and winter sea ice and silicon concentration). Azpeitia tabularis, Hemidiscus cuneiformis and Roperia tesselata were associated ...
format Dataset
author Esper, Oliver
Gersonde, Rainer
Kadagies, Nicole
author_facet Esper, Oliver
Gersonde, Rainer
Kadagies, Nicole
author_sort Esper, Oliver
title Diatom abundance in surface sediments of the Southern Ocean
title_short Diatom abundance in surface sediments of the Southern Ocean
title_full Diatom abundance in surface sediments of the Southern Ocean
title_fullStr Diatom abundance in surface sediments of the Southern Ocean
title_full_unstemmed Diatom abundance in surface sediments of the Southern Ocean
title_sort diatom abundance in surface sediments of the southern ocean
publisher PANGAEA
publishDate 2010
url https://doi.pangaea.de/10.1594/PANGAEA.681699
https://doi.org/10.1594/PANGAEA.681699
op_coverage MEDIAN LATITUDE: -62.043064 * MEDIAN LONGITUDE: -98.422545 * SOUTH-BOUND LATITUDE: -72.052000 * WEST-BOUND LONGITUDE: -120.929500 * NORTH-BOUND LATITUDE: -50.749000 * EAST-BOUND LONGITUDE: -82.220000 * DATE/TIME START: 1994-03-02T05:55:00 * DATE/TIME END: 2001-04-02T14:05:00 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m
long_lat ENVELOPE(-120.929500,-82.220000,-50.749000,-72.052000)
geographic Antarctic
Southern Ocean
The Antarctic
Amundsen Sea
Pacific
geographic_facet Antarctic
Southern Ocean
The Antarctic
Amundsen Sea
Pacific
genre Amundsen Sea
Antarc*
Antarctic
Antarctica
Sea ice
Southern Ocean
genre_facet Amundsen Sea
Antarc*
Antarctic
Antarctica
Sea ice
Southern Ocean
op_source Supplement to: Esper, Oliver; Gersonde, Rainer; Kadagies, Nicole (2010): Diatom distribution in southeastern Pacific surface sediments and their relation to modern environmental variables. Palaeogeography, Palaeoclimatology, Palaeoecology, 287(1-4), 1-27, https://doi.org/10.1016/j.palaeo.2009.12.006
op_relation https://doi.pangaea.de/10.1594/PANGAEA.681699
https://doi.org/10.1594/PANGAEA.681699
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.681699
https://doi.org/10.1016/j.palaeo.2009.12.006
_version_ 1766378823526383616
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.681699 2023-05-15T13:24:20+02:00 Diatom abundance in surface sediments of the Southern Ocean Esper, Oliver Gersonde, Rainer Kadagies, Nicole MEDIAN LATITUDE: -62.043064 * MEDIAN LONGITUDE: -98.422545 * SOUTH-BOUND LATITUDE: -72.052000 * WEST-BOUND LONGITUDE: -120.929500 * NORTH-BOUND LATITUDE: -50.749000 * EAST-BOUND LONGITUDE: -82.220000 * DATE/TIME START: 1994-03-02T05:55:00 * DATE/TIME END: 2001-04-02T14:05:00 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m 2010-02-06 text/tab-separated-values, 2496 data points https://doi.pangaea.de/10.1594/PANGAEA.681699 https://doi.org/10.1594/PANGAEA.681699 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.681699 https://doi.org/10.1594/PANGAEA.681699 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Esper, Oliver; Gersonde, Rainer; Kadagies, Nicole (2010): Diatom distribution in southeastern Pacific surface sediments and their relation to modern environmental variables. Palaeogeography, Palaeoclimatology, Palaeoecology, 287(1-4), 1-27, https://doi.org/10.1016/j.palaeo.2009.12.006 Actinocyclus actinochilus Actinocyclus curvatulus Amundsen Sea ANT-XI/3 ANT-XII/4 ANT-XVIII/5a Asteromphalus hookeri Asteromphalus hyalinus Asteromphalus parvulus AWI_Paleo Azpeitia tabularis var. egregius Azpeitia tabularis var. tabularis Chaetoceros spp. Counting diatoms DEPTH sediment/rock Diatoms indeterminata Elevation of event Eucampia antarctica Event label Fragilariopsis curta Fragilariopsis cylindrus Fragilariopsis doliolus Fragilariopsis kerguelensis Fragilariopsis obliquecostata Fragilariopsis rhombica Fragilariopsis ritscheri Fragilariopsis separanda Fragilariopsis sublinearis Hemidiscus cuneiformis Latitude of event Longitude of event MUC MultiCorer Nitzschia bicapitata Nitzschia kolaczeckii Paleoenvironmental Reconstructions from Marine Sediments @ AWI PLA Plankton net Polarstern Porosira glacialis PS2546-1 PS2547-2 PS2548-2 PS2550-2 PS2657-1 PS2659-2 PS2661-4 Dataset 2010 ftpangaea https://doi.org/10.1594/PANGAEA.681699 https://doi.org/10.1016/j.palaeo.2009.12.006 2023-01-20T08:44:51Z The quantitative analysis of diatom assemblages preserved in 52 samples from the Bellingshausen and the Amundsen Seas provides the first comprehensive view on the distribution of diatoms in surface sediments of the eastern and central Pacific sector of the Southern Ocean. On a latitudinal transect along 120°W, diatom valve accumulation rates (AR) reach maximum values (8–10 × 10**8 valves m**-2 yr**-1) in a zone extending over ca. 900 km between the Antarctic Polar Front and the maximum average winter sea ice extent and exceed those ARs obtained from an eastern transect along 90°W by one order of magnitude. Lowest diatom concentrations (1–3 × 10**6 valves g**-1) were encountered in sediments of the Sea Ice Zone, affected by winter and summer sea ice. The accumulation rate pattern of the most abundant diatom Fragilariopsis kerguelensis (> 50% abundance in 47 samples) mirrors the pattern of the total diatom valve AR and the biogenic silica (BSi) AR, making F. kerguelensis the major contributor to the BSi preserved at the sea floor. Relative abundances of diatom species and species groups were statistically compared with a selection of environmental variables, such as the mean summer sea surface temperature and salinity, mean annual surface nutrient concentration (nitrate, phosphate, silicon), mean annual water column stratification, mixed layer depth in summer, and mean summer and winter sea ice concentrations. Polynomial canonical redundancy analysis (RDA) revealed the biogeographic distribution of diatom species had the strongest relationship with summer sea surface temperature (SSST) out of the nine tested environmental variables. This relationship accounted for 69.6% of the total variance of the diatom distribution, with 29.7% explained by the first gradient (significantly correlated to SSST with r**2 = 0.941) and 15.6% explained by the second gradient (correlated to both summer and winter sea ice and silicon concentration). Azpeitia tabularis, Hemidiscus cuneiformis and Roperia tesselata were associated ... Dataset Amundsen Sea Antarc* Antarctic Antarctica Sea ice Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Southern Ocean The Antarctic Amundsen Sea Pacific ENVELOPE(-120.929500,-82.220000,-50.749000,-72.052000)