Fatty acid patterns of Southern Ocean shelf and deep sea peracarid crustaceans and a possible food source, foraminiferans
In order to investigate the diversity of diet composition in macrobenthic peracarid crustaceans from the Antarctic shelf and deep sea, the fatty acid (FA) composition of different species belonging to the orders Isopoda, Amphipoda, Cumacea and Tanaidacea was analysed. Multivariate analyses of the FA...
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description | In order to investigate the diversity of diet composition in macrobenthic peracarid crustaceans from the Antarctic shelf and deep sea, the fatty acid (FA) composition of different species belonging to the orders Isopoda, Amphipoda, Cumacea and Tanaidacea was analysed. Multivariate analyses of the FA composition confirmed general differences between the orders, but also distinct differences within these orders. To gain information on the origin of the FAs found, the potential food sources sediment, POM and foraminiferans were included in the study. Most of the analysed amphipod species displayed high 18:1(
n−9)–18:1(
n−7) ratios, widely used as an indicator for a carnivorous component in the diet. Cumaceans were characterised by increased phytoplankton FA markers such as 20:5(
n−3) (up to 29% of total FAs), suggesting a diet based on phytodetritus. High values of the FA 20:4(
n−6) were found in some munnopsid isopods (up to 21% of total FAs) and some tanaidacean species (up to 19% of total FAs). 20:4(
n−6) also occurred in high proportions in some foraminiferan samples (up to 21% of total fatty acids), but not in sediment and POM, possibly indicating the ingestion of foraminiferans by some peracarid crustaceans. |
doi_str_mv | 10.1016/j.dsr2.2011.05.013 |
format | Article |
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n−9)–18:1(
n−7) ratios, widely used as an indicator for a carnivorous component in the diet. Cumaceans were characterised by increased phytoplankton FA markers such as 20:5(
n−3) (up to 29% of total FAs), suggesting a diet based on phytodetritus. High values of the FA 20:4(
n−6) were found in some munnopsid isopods (up to 21% of total FAs) and some tanaidacean species (up to 19% of total FAs). 20:4(
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n−9)–18:1(
n−7) ratios, widely used as an indicator for a carnivorous component in the diet. Cumaceans were characterised by increased phytoplankton FA markers such as 20:5(
n−3) (up to 29% of total FAs), suggesting a diet based on phytodetritus. High values of the FA 20:4(
n−6) were found in some munnopsid isopods (up to 21% of total FAs) and some tanaidacean species (up to 19% of total FAs). 20:4(
n−6) also occurred in high proportions in some foraminiferan samples (up to 21% of total fatty acids), but not in sediment and POM, possibly indicating the ingestion of foraminiferans by some peracarid crustaceans.</description><subject>Acetal resins</subject><subject>Crustaceans</subject><subject>Deep sea</subject><subject>Deep sea environments</subject><subject>Diet composition</subject><subject>Diets</subject><subject>Fatty acid</subject><subject>Fatty acids</subject><subject>Foods</subject><subject>Foraminifera</subject><subject>Marine</subject><subject>Peracarida</subject><subject>Sediments</subject><subject>Southern Ocean benthos</subject><issn>0967-0645</issn><issn>1879-0100</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNp9kUGL1TAQx4Mo-Fz9Ap5y04Otk7RNE_Aii6vCwh7Uc0gnEzaPvqYmrfC-vXk-z3uaGeb3Gxj-jL0V0AoQ6uOx9SXLVoIQLQwtiO4ZOwg9mgYEwHN2AKPGBlQ_vGSvSjkCQNcpc2DnO7dtZ-4wer7WlvJSeAr8R9q3xzrwByS38PJIc-Bu8dwTrbyQ4ytlhy5XD_NeNnfhyj-k7lIpcZqJh5Q8L2nPSB_qkN0pLjFUcymv2Yvg5kJv_tcb9uvuy8_bb839w9fvt5_vG-w7sTWoQWkJiOi1m5QGLbUMk6NpdEqiD513MihjOqMnpwhHAjl4QxjEhAK7G_buenfN6fdOZbOnWJDm2S2U9mK1MWLQqu8q-f5JUqhR9MPQa6iovKKY66uZgl1zPLl8tgLsJRF7tJdE7CURC4OtiVTp01Wi-u6fSNkWjLQg-ZgJN-tTfEr_Cx0Ulmo</recordid><startdate>20111001</startdate><enddate>20111001</enddate><creator>Würzberg, Laura</creator><creator>Peters, Janna</creator><creator>Brandt, Angelika</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>20111001</creationdate><title>Fatty acid patterns of Southern Ocean shelf and deep sea peracarid crustaceans and a possible food source, foraminiferans</title><author>Würzberg, Laura ; Peters, Janna ; Brandt, Angelika</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c431t-c806820cccd8ab6808282fbaeb7a62cdf3da2f699398ba6ec7e025d9ecf1bc1c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Acetal resins</topic><topic>Crustaceans</topic><topic>Deep sea</topic><topic>Deep sea environments</topic><topic>Diet composition</topic><topic>Diets</topic><topic>Fatty acid</topic><topic>Fatty acids</topic><topic>Foods</topic><topic>Foraminifera</topic><topic>Marine</topic><topic>Peracarida</topic><topic>Sediments</topic><topic>Southern Ocean benthos</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Würzberg, Laura</creatorcontrib><creatorcontrib>Peters, Janna</creatorcontrib><creatorcontrib>Brandt, Angelika</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Deep-sea research. Part II, Topical studies in oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Würzberg, Laura</au><au>Peters, Janna</au><au>Brandt, Angelika</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Fatty acid patterns of Southern Ocean shelf and deep sea peracarid crustaceans and a possible food source, foraminiferans</atitle><jtitle>Deep-sea research. Part II, Topical studies in oceanography</jtitle><date>2011-10-01</date><risdate>2011</risdate><volume>58</volume><issue>19</issue><spage>2027</spage><epage>2035</epage><pages>2027-2035</pages><issn>0967-0645</issn><eissn>1879-0100</eissn><abstract>In order to investigate the diversity of diet composition in macrobenthic peracarid crustaceans from the Antarctic shelf and deep sea, the fatty acid (FA) composition of different species belonging to the orders Isopoda, Amphipoda, Cumacea and Tanaidacea was analysed. Multivariate analyses of the FA composition confirmed general differences between the orders, but also distinct differences within these orders. To gain information on the origin of the FAs found, the potential food sources sediment, POM and foraminiferans were included in the study. Most of the analysed amphipod species displayed high 18:1(
n−9)–18:1(
n−7) ratios, widely used as an indicator for a carnivorous component in the diet. Cumaceans were characterised by increased phytoplankton FA markers such as 20:5(
n−3) (up to 29% of total FAs), suggesting a diet based on phytodetritus. High values of the FA 20:4(
n−6) were found in some munnopsid isopods (up to 21% of total FAs) and some tanaidacean species (up to 19% of total FAs). 20:4(
n−6) also occurred in high proportions in some foraminiferan samples (up to 21% of total fatty acids), but not in sediment and POM, possibly indicating the ingestion of foraminiferans by some peracarid crustaceans.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.dsr2.2011.05.013</doi><tpages>9</tpages></addata></record> |
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subjects | Acetal resins Crustaceans Deep sea Deep sea environments Diet composition Diets Fatty acid Fatty acids Foods Foraminifera Marine Peracarida Sediments Southern Ocean benthos |
title | Fatty acid patterns of Southern Ocean shelf and deep sea peracarid crustaceans and a possible food source, foraminiferans |
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