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Chlorophyll a in Antarctic sea ice from historical ice core data

Identifieur interne : 002500 ( Istex/Corpus ); précédent : 002499; suivant : 002501

Chlorophyll a in Antarctic sea ice from historical ice core data

Auteurs : K. M. Meiners ; M. Vancoppenolle ; S. Thanassekos ; G. S. Dieckmann ; D. N. Thomas ; J. Tison ; K. R. Arrigo ; D. L. Garrison ; A. Mcminn ; D. Lannuzel ; P. Van Der Merwe ; K. M. Swadling ; W. O. Smith Jr. ; I. Melnikov ; B. Raymond

Source :

RBID : ISTEX:C7867B31907A9DE9C8AEEA1C18634636EAC1EB76

English descriptors

Abstract

Sea ice core chlorophyll a data are used to describe the seasonal, regional and vertical distribution of algal biomass in Southern Ocean pack ice. The Antarctic Sea Ice Processes and Climate – Biology (ASPeCt – Bio) circumpolar dataset consists of 1300 ice cores collected during 32 cruises over a period of 25 years. The analyses show that integrated sea ice chlorophyll apeaks in early spring and late austral summer, which is consistent with theories on light and nutrient limitation. The results indicate that on a circum‐Antarctic scale, surface, internal and bottom sea ice layers contribute equally to integrated biomass, but vertical distribution shows distinct differences among six regions around the continent. The vertical distribution of sea ice algal biomass depends on sea ice thickness, with surface communities most commonly associated with thin ice (<0.4 m), and ice of moderate thickness (0.4–1.0 m) having the highest probability of forming bottom communities.

Url:
DOI: 10.1029/2012GL053478

Links to Exploration step

ISTEX:C7867B31907A9DE9C8AEEA1C18634636EAC1EB76

Le document en format XML

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<div type="abstract">Sea ice core chlorophyll a data are used to describe the seasonal, regional and vertical distribution of algal biomass in Southern Ocean pack ice. The Antarctic Sea Ice Processes and Climate – Biology (ASPeCt – Bio) circumpolar dataset consists of 1300 ice cores collected during 32 cruises over a period of 25 years. The analyses show that integrated sea ice chlorophyll apeaks in early spring and late austral summer, which is consistent with theories on light and nutrient limitation. The results indicate that on a circum‐Antarctic scale, surface, internal and bottom sea ice layers contribute equally to integrated biomass, but vertical distribution shows distinct differences among six regions around the continent. The vertical distribution of sea ice algal biomass depends on sea ice thickness, with surface communities most commonly associated with thin ice (<0.4 m), and ice of moderate thickness (0.4–1.0 m) having the highest probability of forming bottom communities.</div>
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<p xml:id="grl29738-para-0004">Sea ice core chlorophyll
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<correspondenceTo>Corresponding author: K. M. Meiners, Australian Antarctic Division, Department of Sustainability, Environment, Water, Population and Communities, Channel Highway, Kingston, TAS 7050, Australia. (
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<affiliation>Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Tasmania, Australia</affiliation>
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<publisher>Blackwell Publishing Ltd</publisher>
<dateIssued encoding="w3cdtf">2012-11</dateIssued>
<dateCaptured encoding="w3cdtf">2012-08-05</dateCaptured>
<dateValid encoding="w3cdtf">2012-09-20</dateValid>
<edition>Meiners, K. M., et al. (2012), Chlorophyll a in Antarctic sea ice from historical ice core data, Geophys. Res. Lett., 39, L21602, doi:10.1029/2012GL053478.</edition>
<copyrightDate encoding="w3cdtf">2012</copyrightDate>
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<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
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<abstract>Sea ice core chlorophyll a data are used to describe the seasonal, regional and vertical distribution of algal biomass in Southern Ocean pack ice. The Antarctic Sea Ice Processes and Climate – Biology (ASPeCt – Bio) circumpolar dataset consists of 1300 ice cores collected during 32 cruises over a period of 25 years. The analyses show that integrated sea ice chlorophyll apeaks in early spring and late austral summer, which is consistent with theories on light and nutrient limitation. The results indicate that on a circum‐Antarctic scale, surface, internal and bottom sea ice layers contribute equally to integrated biomass, but vertical distribution shows distinct differences among six regions around the continent. The vertical distribution of sea ice algal biomass depends on sea ice thickness, with surface communities most commonly associated with thin ice (<0.4 m), and ice of moderate thickness (0.4–1.0 m) having the highest probability of forming bottom communities.</abstract>
<abstract type="short">Antarctic sea ice chlorophyll a shows maxima in early spring and late summer Surface, internal and bottom ice layers contribute equally to integrated biomass The vertical distribution of chlorophyll a critically depends on ice thickness</abstract>
<subject>
<genre>keywords</genre>
<topic>Antarctica</topic>
<topic>algae</topic>
<topic>biomass</topic>
<topic>chlorophyll a</topic>
<topic>sea ice</topic>
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<title>Geophysical Research Letters</title>
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<title>Geophys. Res. Lett.</title>
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<note type="content"> Auxiliary material for this article contains a text file with a table of voyages compiled in the ASPeCt – Bio database, a figure with three example cores from the Weddell Sea, and a figure of mean normalized chl‐a profiles. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). Additional file information is provided in the readme.txt. Auxiliary material for this article contains a text file with a table of voyages compiled in the ASPeCt – Bio database, a figure with three example cores from the Weddell Sea, and a figure of mean normalized chl‐a profiles. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). Additional file information is provided in the readme.txt. Auxiliary material for this article contains a text file with a table of voyages compiled in the ASPeCt – Bio database, a figure with three example cores from the Weddell Sea, and a figure of mean normalized chl‐a profiles. Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right‐click and select “Save Target As…” (PC) or CTRL‐click and select “Download Link to Disk” (Mac). Additional file information is provided in the readme.txt.Supporting Info Item: readme.txt - Text S1. Description of methods used to create and , with Table S1. - Figure S1. Three example cores from the Weddell Sea. - Figure S2. Mean normalized chl‐a profiles for the complete dataset, profiles classified as surface type, profiles classified as internal type, and profiles classified as bottom type. - Tab‐delimited Table 1. - Tab‐delimited Table 2. - </note>
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<topic authorityURI="http://psi.agu.org/taxonomy5/0400">BIOGEOSCIENCES</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0414">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0434">Data sets</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0442">Estuarine and nearshore processes</topic>
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<topic authorityURI="http://psi.agu.org/taxonomy5/0700">CRYOSPHERE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0750">Sea ice</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/0793">Biogeochemistry</topic>
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<topic authorityURI="http://psi.agu.org/taxonomy5/1600">GLOBAL CHANGE</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1615">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/1615">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4200">OCEANOGRAPHY: GENERAL</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4235">Estuarine processes</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4500">OCEANOGRAPHY: PHYSICAL</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4540">Ice mechanics and air/sea/ice exchange processes</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4800">OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4805">Biogeochemical cycles, processes, and modeling</topic>
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<topic authorityURI="http://psi.agu.org/taxonomy5/4900">PALEOCEANOGRAPHY</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4912">Biogeochemical cycles, processes, and modeling</topic>
<topic authorityURI="http://psi.agu.org/taxonomy5/4912">Biogeochemical cycles, processes, and modeling</topic>
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<subject>
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<topic>Oceans</topic>
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<identifier type="ISSN">0094-8276</identifier>
<identifier type="eISSN">1944-8007</identifier>
<identifier type="DOI">10.1002/(ISSN)1944-8007</identifier>
<identifier type="CODEN">GPRLAJ</identifier>
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<part>
<date>2012</date>
<detail type="volume">
<caption>vol.</caption>
<number>39</number>
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<caption>no.</caption>
<number>21</number>
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<identifier type="DOI">10.1029/2012GL053478</identifier>
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<accessCondition type="use and reproduction" contentType="copyright">©2012. American Geophysical Union. All Rights Reserved.</accessCondition>
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