Seasonal variation in stable C and N isotope ratios of the Rhone River inputs to the Mediterranean Sea (2004-2005)
The temporal variation in the stable carbon and nitrogen isotope ratios of particulate organic matter (POM) in the Rhone River was investigated on a monthly basis during a 2-year period (2004-2005). In spite of high month-to-month variation, interannually consistent seasonal trends appeared, with si...
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| Veröffentlicht in: | Biogeochemistry 2010-09, Vol.100 (1-3), p.139-150 |
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| creator | Harmelin-Vivien, M Dierking, J Bănaru, D Fontaine, M. F Arlhac, D |
| description | The temporal variation in the stable carbon and nitrogen isotope ratios of particulate organic matter (POM) in the Rhone River was investigated on a monthly basis during a 2-year period (2004-2005). In spite of high month-to-month variation, interannually consistent seasonal trends appeared, with significantly lower δ¹³C (8) values, and lower %C, %N, and chlorophylls concentrations indicated the predominance of allochthonous terrestrial detritus material in the river POM. The lower δ¹³C values recorded in spring-summer, when the phytoplankton biomass was high, were related to the lower carbon isotopic signatures of freshwater diatoms and chlorophytes compared to those of terrestrial plants. Overall, Rhone River POM was mainly composed of terrestrially derived material (90%), with autochthonous phytoplankton representing only 10% as a mean, in spite of a higher mean contribution of phytoplankton (27%) to river POM in summer. |
| doi_str_mv | 10.1007/s10533-010-9411-z |
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F ; Arlhac, D</creator><creatorcontrib>Harmelin-Vivien, M ; Dierking, J ; Bănaru, D ; Fontaine, M. F ; Arlhac, D</creatorcontrib><description>The temporal variation in the stable carbon and nitrogen isotope ratios of particulate organic matter (POM) in the Rhone River was investigated on a monthly basis during a 2-year period (2004-2005). In spite of high month-to-month variation, interannually consistent seasonal trends appeared, with significantly lower δ¹³C (<−28.2‰) in spring than in the other seasons. In contrast, δ¹⁵N did not exhibit significant temporal variation. In spring and summer, high chlorophyll a and b concentrations were associated with low C/N values (<8) and a high percentage of organic carbon (%C) and organic nitrogen (%N), testifying to high development of autochthonous riverine phytoplankton (mainly diatoms and chlorophytes). In fall and winter, higher δ¹³C (>−27.2‰) and C/N (>8) values, and lower %C, %N, and chlorophylls concentrations indicated the predominance of allochthonous terrestrial detritus material in the river POM. The lower δ¹³C values recorded in spring-summer, when the phytoplankton biomass was high, were related to the lower carbon isotopic signatures of freshwater diatoms and chlorophytes compared to those of terrestrial plants. Overall, Rhone River POM was mainly composed of terrestrially derived material (90%), with autochthonous phytoplankton representing only 10% as a mean, in spite of a higher mean contribution of phytoplankton (27%) to river POM in summer.</description><identifier>ISSN: 0168-2563</identifier><identifier>EISSN: 1573-515X</identifier><identifier>DOI: 10.1007/s10533-010-9411-z</identifier><identifier>CODEN: BIOGEP</identifier><language>eng</language><publisher>Dordrecht: Dordrecht : Springer Netherlands</publisher><subject>Animal and plant ecology ; Animal, plant and microbial ecology ; Bacillariophyceae ; Biochemistry ; Biodiversity and Ecology ; Biogeosciences ; Biological and medical sciences ; C/N ; Carbon ; chlorophyll ; Chlorophylls ; Detritus ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Ecosystems ; Environmental Chemistry ; Environmental Sciences ; Exact sciences and technology ; Fresh water ; Freshwater organic matter ; Fundamental and applied biological sciences. Psychology ; Geochemistry ; Gulf of Lions ; Hydrology ; Hydrology. Hydrogeology ; Isotopes ; Life Sciences ; Mineralogy ; Nitrogen ; Organic carbon ; Organic nitrogen ; Particulate matter ; Particulate organic matter ; Phytoplankton ; River water ; Rivers ; Sea water ecosystems ; Seas ; Seasonal variations ; Seasons ; Signatures ; Silicates ; Spring ; stable isotopes ; Summer ; Synecology ; Water geochemistry</subject><ispartof>Biogeochemistry, 2010-09, Vol.100 (1-3), p.139-150</ispartof><rights>2010 Springer</rights><rights>Springer Science+Business Media B.V. 2010</rights><rights>2015 INIST-CNRS</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c457t-ec724e797154dad3e415d33daeca237dcdea7ad4ebededddcd5a4715a7f82ad23</citedby><cites>FETCH-LOGICAL-c457t-ec724e797154dad3e415d33daeca237dcdea7ad4ebededddcd5a4715a7f82ad23</cites><orcidid>0000-0003-3085-2899 ; 0000-0002-8126-4328</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/40800614$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/40800614$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,776,780,799,881,27901,27902,41464,42533,51294,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=23195566$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-01833600$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Harmelin-Vivien, M</creatorcontrib><creatorcontrib>Dierking, J</creatorcontrib><creatorcontrib>Bănaru, D</creatorcontrib><creatorcontrib>Fontaine, M. F</creatorcontrib><creatorcontrib>Arlhac, D</creatorcontrib><title>Seasonal variation in stable C and N isotope ratios of the Rhone River inputs to the Mediterranean Sea (2004-2005)</title><title>Biogeochemistry</title><addtitle>Biogeochemistry</addtitle><description>The temporal variation in the stable carbon and nitrogen isotope ratios of particulate organic matter (POM) in the Rhone River was investigated on a monthly basis during a 2-year period (2004-2005). In spite of high month-to-month variation, interannually consistent seasonal trends appeared, with significantly lower δ¹³C (<−28.2‰) in spring than in the other seasons. In contrast, δ¹⁵N did not exhibit significant temporal variation. In spring and summer, high chlorophyll a and b concentrations were associated with low C/N values (<8) and a high percentage of organic carbon (%C) and organic nitrogen (%N), testifying to high development of autochthonous riverine phytoplankton (mainly diatoms and chlorophytes). In fall and winter, higher δ¹³C (>−27.2‰) and C/N (>8) values, and lower %C, %N, and chlorophylls concentrations indicated the predominance of allochthonous terrestrial detritus material in the river POM. The lower δ¹³C values recorded in spring-summer, when the phytoplankton biomass was high, were related to the lower carbon isotopic signatures of freshwater diatoms and chlorophytes compared to those of terrestrial plants. Overall, Rhone River POM was mainly composed of terrestrially derived material (90%), with autochthonous phytoplankton representing only 10% as a mean, in spite of a higher mean contribution of phytoplankton (27%) to river POM in summer.</description><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Bacillariophyceae</subject><subject>Biochemistry</subject><subject>Biodiversity and Ecology</subject><subject>Biogeosciences</subject><subject>Biological and medical sciences</subject><subject>C/N</subject><subject>Carbon</subject><subject>chlorophyll</subject><subject>Chlorophylls</subject><subject>Detritus</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Ecosystems</subject><subject>Environmental Chemistry</subject><subject>Environmental Sciences</subject><subject>Exact sciences and technology</subject><subject>Fresh water</subject><subject>Freshwater organic matter</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Geochemistry</subject><subject>Gulf of Lions</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Isotopes</subject><subject>Life Sciences</subject><subject>Mineralogy</subject><subject>Nitrogen</subject><subject>Organic carbon</subject><subject>Organic nitrogen</subject><subject>Particulate matter</subject><subject>Particulate organic matter</subject><subject>Phytoplankton</subject><subject>River water</subject><subject>Rivers</subject><subject>Sea water ecosystems</subject><subject>Seas</subject><subject>Seasonal variations</subject><subject>Seasons</subject><subject>Signatures</subject><subject>Silicates</subject><subject>Spring</subject><subject>stable isotopes</subject><subject>Summer</subject><subject>Synecology</subject><subject>Water geochemistry</subject><issn>0168-2563</issn><issn>1573-515X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kV1rFDEUhgex4Fr9AV6IQRDtxejJ12TmsixqhVXBWvAunE7OdGeZTrZJdsH--macskIvepOQnOe87_koilccPnIA8yly0FKWwKFsFOfl7ZNiwbWRpeb6z9NiAbyqS6Er-ax4HuMGABoDclGEc8LoRxzYHkOPqfcj60cWE14OxJYMR8d-sD765LfEwgRE5juW1sR-rf2Yz35PIedsdymy5P9FvpPrE4WAI-HIsgX7IABUmQ998qI46nCI9PL-Pi4uvnz-vTwrVz-_fluerspWaZNKao1QZBrDtXLoJCmunZQOqUUhjWsdoUGn6JIcOZffGlWG0XS1QCfkcXEy665xsNvQX2P4az329ux0Zac_4LWUFcCeZ_b9zG6Dv9lRTPa6jy0NQ-7A76Ktuday0kJl8u0DcuN3IQ8wWqOaptE1n6z5DLXBxxioO_hzsNO-7LyvXALYaV_2Nue8uxfG2OLQ5eG1fTwkCskbrasqc2LmYg6NVxT-F_CY-Os5aROTDwdRBTVAxaeu3szxDr3Fq5CNL84FcJlnVGtRCXkHPP-2vQ</recordid><startdate>20100901</startdate><enddate>20100901</enddate><creator>Harmelin-Vivien, M</creator><creator>Dierking, J</creator><creator>Bănaru, D</creator><creator>Fontaine, M. 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F</au><au>Arlhac, D</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seasonal variation in stable C and N isotope ratios of the Rhone River inputs to the Mediterranean Sea (2004-2005)</atitle><jtitle>Biogeochemistry</jtitle><stitle>Biogeochemistry</stitle><date>2010-09-01</date><risdate>2010</risdate><volume>100</volume><issue>1-3</issue><spage>139</spage><epage>150</epage><pages>139-150</pages><issn>0168-2563</issn><eissn>1573-515X</eissn><coden>BIOGEP</coden><abstract>The temporal variation in the stable carbon and nitrogen isotope ratios of particulate organic matter (POM) in the Rhone River was investigated on a monthly basis during a 2-year period (2004-2005). In spite of high month-to-month variation, interannually consistent seasonal trends appeared, with significantly lower δ¹³C (<−28.2‰) in spring than in the other seasons. In contrast, δ¹⁵N did not exhibit significant temporal variation. In spring and summer, high chlorophyll a and b concentrations were associated with low C/N values (<8) and a high percentage of organic carbon (%C) and organic nitrogen (%N), testifying to high development of autochthonous riverine phytoplankton (mainly diatoms and chlorophytes). In fall and winter, higher δ¹³C (>−27.2‰) and C/N (>8) values, and lower %C, %N, and chlorophylls concentrations indicated the predominance of allochthonous terrestrial detritus material in the river POM. The lower δ¹³C values recorded in spring-summer, when the phytoplankton biomass was high, were related to the lower carbon isotopic signatures of freshwater diatoms and chlorophytes compared to those of terrestrial plants. Overall, Rhone River POM was mainly composed of terrestrially derived material (90%), with autochthonous phytoplankton representing only 10% as a mean, in spite of a higher mean contribution of phytoplankton (27%) to river POM in summer.</abstract><cop>Dordrecht</cop><pub>Dordrecht : Springer Netherlands</pub><doi>10.1007/s10533-010-9411-z</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0003-3085-2899</orcidid><orcidid>https://orcid.org/0000-0002-8126-4328</orcidid></addata></record> |
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| subjects | Animal and plant ecology Animal, plant and microbial ecology Bacillariophyceae Biochemistry Biodiversity and Ecology Biogeosciences Biological and medical sciences C/N Carbon chlorophyll Chlorophylls Detritus Earth and Environmental Science Earth Sciences Earth, ocean, space Ecosystems Environmental Chemistry Environmental Sciences Exact sciences and technology Fresh water Freshwater organic matter Fundamental and applied biological sciences. Psychology Geochemistry Gulf of Lions Hydrology Hydrology. Hydrogeology Isotopes Life Sciences Mineralogy Nitrogen Organic carbon Organic nitrogen Particulate matter Particulate organic matter Phytoplankton River water Rivers Sea water ecosystems Seas Seasonal variations Seasons Signatures Silicates Spring stable isotopes Summer Synecology Water geochemistry |
| title | Seasonal variation in stable C and N isotope ratios of the Rhone River inputs to the Mediterranean Sea (2004-2005) |
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