Plankton community composition, organic carbon and thorium-234 particle size distributions, and particle export in the Sargasso Sea
Measurements of plankton community composition (eight planktonic groups), particle size-fractionated (10, 20, 53, 70, and 100-μm Nitex screens) distributions of organic carbon (OC) and 234Th, and particle export of OC and 234Th are reported over a seasonal cycle (2006-2007) from the Bermuda Atlantic...
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creator | Brew, H. S. Moran, S. B. Lomas, M. W. Burd, A. B. |
description | Measurements of plankton community composition (eight planktonic groups), particle size-fractionated (10, 20, 53, 70, and 100-μm Nitex screens) distributions of organic carbon (OC) and 234Th, and particle export of OC and 234Th are reported over a seasonal cycle
(2006-2007) from the Bermuda Atlantic Time-Series (BATS) site. Results indicate a convergence of the particle size distributions of OC and 234Th during the winter-spring bloom period (January-March, 2007). The observed convergence of these particle size distributions
is directly correlated to the depth-integrated abundance of autotrophic pico-eukaryotes (r = 0.97, P < 0.05) and, to a lesser extent, Synechococcus (r = 0.85, P < 0.14). In addition, there are positive correlations between the sediment trap flux of OC and 234Th at 150
m and the depth-integrated abundance of pico-eukaryotes (r = 0.94, P < 0.06 for OC, and r = 0.98, P < 0.05 for 234Th) and Synechococcus (r = 0.95, P < 0.05 for OC, and r = 0.94, P < 0.06 for 234Th). An implication of these observations and recent modeling
studies (Richardson and Jackson, 2007) is that, although small in size, pico-plankton may influence large particle export from the surface waters of the subtropical Atlantic. |
doi_str_mv | 10.1357/002224009792006124 |
format | Article |
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(2006-2007) from the Bermuda Atlantic Time-Series (BATS) site. Results indicate a convergence of the particle size distributions of OC and 234Th during the winter-spring bloom period (January-March, 2007). The observed convergence of these particle size distributions
is directly correlated to the depth-integrated abundance of autotrophic pico-eukaryotes (r = 0.97, P < 0.05) and, to a lesser extent, Synechococcus (r = 0.85, P < 0.14). In addition, there are positive correlations between the sediment trap flux of OC and 234Th at 150
m and the depth-integrated abundance of pico-eukaryotes (r = 0.94, P < 0.06 for OC, and r = 0.98, P < 0.05 for 234Th) and Synechococcus (r = 0.95, P < 0.05 for OC, and r = 0.94, P < 0.06 for 234Th). An implication of these observations and recent modeling
studies (Richardson and Jackson, 2007) is that, although small in size, pico-plankton may influence large particle export from the surface waters of the subtropical Atlantic.]]></description><identifier>ISSN: 0022-2402</identifier><identifier>EISSN: 1543-9542</identifier><identifier>DOI: 10.1357/002224009792006124</identifier><identifier>CODEN: JMMRAO</identifier><language>eng</language><publisher>New Haven: Sears Foundation for Marine Research</publisher><subject>Chemical elements ; Hydrologic cycle ; Hydrologic modeling ; Marine ; Ocean-atmosphere interaction ; Oceanography ; Organic chemicals ; Plankton ; Synechococcus</subject><ispartof>Journal of marine research, 2009-11, Vol.67 (6), p.845-868</ispartof><rights>Copyright Sears Foundation for Marine Research Nov 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c432t-44cc6560676870ec7b3471e567d198d076399b3e0e9898e8f12b3983613eb2333</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,782,786,27931,27932</link.rule.ids></links><search><creatorcontrib>Brew, H. S.</creatorcontrib><creatorcontrib>Moran, S. B.</creatorcontrib><creatorcontrib>Lomas, M. W.</creatorcontrib><creatorcontrib>Burd, A. B.</creatorcontrib><title>Plankton community composition, organic carbon and thorium-234 particle size distributions, and particle export in the Sargasso Sea</title><title>Journal of marine research</title><addtitle>J Mar Res</addtitle><description><![CDATA[Measurements of plankton community composition (eight planktonic groups), particle size-fractionated (10, 20, 53, 70, and 100-μm Nitex screens) distributions of organic carbon (OC) and 234Th, and particle export of OC and 234Th are reported over a seasonal cycle
(2006-2007) from the Bermuda Atlantic Time-Series (BATS) site. Results indicate a convergence of the particle size distributions of OC and 234Th during the winter-spring bloom period (January-March, 2007). The observed convergence of these particle size distributions
is directly correlated to the depth-integrated abundance of autotrophic pico-eukaryotes (r = 0.97, P < 0.05) and, to a lesser extent, Synechococcus (r = 0.85, P < 0.14). In addition, there are positive correlations between the sediment trap flux of OC and 234Th at 150
m and the depth-integrated abundance of pico-eukaryotes (r = 0.94, P < 0.06 for OC, and r = 0.98, P < 0.05 for 234Th) and Synechococcus (r = 0.95, P < 0.05 for OC, and r = 0.94, P < 0.06 for 234Th). An implication of these observations and recent modeling
studies (Richardson and Jackson, 2007) is that, although small in size, pico-plankton may influence large particle export from the surface waters of the subtropical Atlantic.]]></description><subject>Chemical elements</subject><subject>Hydrologic cycle</subject><subject>Hydrologic modeling</subject><subject>Marine</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceanography</subject><subject>Organic chemicals</subject><subject>Plankton</subject><subject>Synechococcus</subject><issn>0022-2402</issn><issn>1543-9542</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNp1kVGLFSEYhiUKOm39ga6km252Nv10dLyKWKoNNgq2rsVxPCdPMzqpE-3e9sdzzjkUFAnqJzzvo3wi9JSSC8pa-YIQAOCEKKmAEEGB30Mb2nLWqJbDfbRZgaYS8BA9ynlfj4ILuUE_P44mfC0xYBunaQm-3K7VHLMvPoZzHNPOBG-xNamvlAkDLl9i8svUAON4Nql4Ozqc_Z3Dg88l-X5Zo_n8AP8G3I85poJ9qHmHb0z15hzxjTOP0YOtGbN7ctrP0Oc3rz9dXjXXH96-u3x13VjOoDScWytaQYQUnSTOyp5xSV0r5EBVNxApmFI9c8SpTnWu21LomeqYoMz1wBg7Q8-P3jnFb4vLRU8-WzfWDri4ZK0IMCkldJV89he5j0sK9XFactkCZ7KtEBwhm2LOyW31nPxk0q2mRK-_ov_9lRp6eQz5sHOhmD_i_ZQOs5KqJtch5KkgQtc2HopqeP8fg7cHwelW0N-FDKL6gBIFoGlbl8FtzTIWXUzSuzudBfsFB9qsig</recordid><startdate>20091101</startdate><enddate>20091101</enddate><creator>Brew, H. S.</creator><creator>Moran, S. B.</creator><creator>Lomas, M. W.</creator><creator>Burd, A. B.</creator><general>Sears Foundation for Marine Research</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>SOI</scope><scope>7SN</scope><scope>8FD</scope><scope>FR3</scope><scope>H99</scope><scope>L.F</scope><scope>P64</scope></search><sort><creationdate>20091101</creationdate><title>Plankton community composition, organic carbon and thorium-234 particle size distributions, and particle export in the Sargasso Sea</title><author>Brew, H. S. ; Moran, S. B. ; Lomas, M. W. ; Burd, A. B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c432t-44cc6560676870ec7b3471e567d198d076399b3e0e9898e8f12b3983613eb2333</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Chemical elements</topic><topic>Hydrologic cycle</topic><topic>Hydrologic modeling</topic><topic>Marine</topic><topic>Ocean-atmosphere interaction</topic><topic>Oceanography</topic><topic>Organic chemicals</topic><topic>Plankton</topic><topic>Synechococcus</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Brew, H. S.</creatorcontrib><creatorcontrib>Moran, S. B.</creatorcontrib><creatorcontrib>Lomas, M. W.</creatorcontrib><creatorcontrib>Burd, A. B.</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><collection>Ecology Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>ASFA: Marine Biotechnology Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Marine Biotechnology Abstracts</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>Journal of marine research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Brew, H. S.</au><au>Moran, S. B.</au><au>Lomas, M. W.</au><au>Burd, A. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Plankton community composition, organic carbon and thorium-234 particle size distributions, and particle export in the Sargasso Sea</atitle><jtitle>Journal of marine research</jtitle><stitle>J Mar Res</stitle><date>2009-11-01</date><risdate>2009</risdate><volume>67</volume><issue>6</issue><spage>845</spage><epage>868</epage><pages>845-868</pages><issn>0022-2402</issn><eissn>1543-9542</eissn><coden>JMMRAO</coden><abstract><![CDATA[Measurements of plankton community composition (eight planktonic groups), particle size-fractionated (10, 20, 53, 70, and 100-μm Nitex screens) distributions of organic carbon (OC) and 234Th, and particle export of OC and 234Th are reported over a seasonal cycle
(2006-2007) from the Bermuda Atlantic Time-Series (BATS) site. Results indicate a convergence of the particle size distributions of OC and 234Th during the winter-spring bloom period (January-March, 2007). The observed convergence of these particle size distributions
is directly correlated to the depth-integrated abundance of autotrophic pico-eukaryotes (r = 0.97, P < 0.05) and, to a lesser extent, Synechococcus (r = 0.85, P < 0.14). In addition, there are positive correlations between the sediment trap flux of OC and 234Th at 150
m and the depth-integrated abundance of pico-eukaryotes (r = 0.94, P < 0.06 for OC, and r = 0.98, P < 0.05 for 234Th) and Synechococcus (r = 0.95, P < 0.05 for OC, and r = 0.94, P < 0.06 for 234Th). An implication of these observations and recent modeling
studies (Richardson and Jackson, 2007) is that, although small in size, pico-plankton may influence large particle export from the surface waters of the subtropical Atlantic.]]></abstract><cop>New Haven</cop><pub>Sears Foundation for Marine Research</pub><doi>10.1357/002224009792006124</doi><tpages>24</tpages></addata></record> |
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subjects | Chemical elements Hydrologic cycle Hydrologic modeling Marine Ocean-atmosphere interaction Oceanography Organic chemicals Plankton Synechococcus |
title | Plankton community composition, organic carbon and thorium-234 particle size distributions, and particle export in the Sargasso Sea |
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