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Glomalin-related soil protein deposition and carbon sequestration in the Old Yellow River delta.

Identifieur interne : 000948 ( Main/Exploration ); précédent : 000947; suivant : 000949

Glomalin-related soil protein deposition and carbon sequestration in the Old Yellow River delta.

Auteurs : Qiang Wang [République populaire de Chine] ; Junwei Li [République populaire de Chine] ; Jingyan Chen [République populaire de Chine] ; Hualong Hong [République populaire de Chine] ; Haoliang Lu [République populaire de Chine] ; Jingchun Liu [République populaire de Chine] ; Yunwei Dong [République populaire de Chine] ; Chongling Yan [République populaire de Chine]

Source :

RBID : pubmed:29304499

Descripteurs français

English descriptors

Abstract

Glomalin-related soil protein (GRSP), a particular terrigenous-derived carbon (C), is transported to the coastal oceans, where it accumulates in sediments. We hypothesized that terrigenous C (GRSP) accumulation could enhance marine C sequestration, and sediment fertility would increase the C stock in the marine ecosystem. In this study, we tested GRSP contribution to marine sediment C, nitrogen (N) and iron (Fe), and explored whether GRSP deposition varied with sediment fertility levels in the Old Yellow River delta. The mean concentration of total GRSP was 1.10±0.04mgg-1 (0.24MgCha-1), accounting for 6.41±0.17% of total organic C and 3.75±0.13% of total N in the 0-10cm marine sediments, indicating that the coastal marine system is an important sink of GRSP. GRSP also contained 1.46±0.06% Fe (20.7kgFeha-1), accounting for 0.058±0.003% of total Fe in marine sediments. Meanwhile, Fe-content in GRSP significantly decreased with distance from the shore, indicating that Fe was released with GRSP transfer and thus GRSP was a new natural Fe fertilization in marine environment. Furthermore, GRSP enhanced marine C sequestration by its rapid deposition and Fe contribution. Combined indicators of sediment fertility (factor 1) were significantly positively correlated with GRSP concentrations by Principal Component Analysis. Co-deposited with nutrient elements, GRSP fractions were accumulated more in more fertile sediments but less in less fertile sediments. GRSP, a mixture of co-existent multiple elements, can be used as a nutrient controlled-release agent in the marine ecosystem. GRSP fractions were responsive to marine sediment fertility levels and the understanding of their function in sediment C sequestration will provide new insights into the importance of terrestrial-marine linkages.

DOI: 10.1016/j.scitotenv.2017.12.303
PubMed: 29304499


Affiliations:


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Le document en format XML

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<term>Fungal Proteins (chemistry)</term>
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<div type="abstract" xml:lang="en">Glomalin-related soil protein (GRSP), a particular terrigenous-derived carbon (C), is transported to the coastal oceans, where it accumulates in sediments. We hypothesized that terrigenous C (GRSP) accumulation could enhance marine C sequestration, and sediment fertility would increase the C stock in the marine ecosystem. In this study, we tested GRSP contribution to marine sediment C, nitrogen (N) and iron (Fe), and explored whether GRSP deposition varied with sediment fertility levels in the Old Yellow River delta. The mean concentration of total GRSP was 1.10±0.04mgg
<sup>-1</sup>
(0.24MgCha
<sup>-1</sup>
), accounting for 6.41±0.17% of total organic C and 3.75±0.13% of total N in the 0-10cm marine sediments, indicating that the coastal marine system is an important sink of GRSP. GRSP also contained 1.46±0.06% Fe (20.7kgFeha
<sup>-1</sup>
), accounting for 0.058±0.003% of total Fe in marine sediments. Meanwhile, Fe-content in GRSP significantly decreased with distance from the shore, indicating that Fe was released with GRSP transfer and thus GRSP was a new natural Fe fertilization in marine environment. Furthermore, GRSP enhanced marine C sequestration by its rapid deposition and Fe contribution. Combined indicators of sediment fertility (factor 1) were significantly positively correlated with GRSP concentrations by Principal Component Analysis. Co-deposited with nutrient elements, GRSP fractions were accumulated more in more fertile sediments but less in less fertile sediments. GRSP, a mixture of co-existent multiple elements, can be used as a nutrient controlled-release agent in the marine ecosystem. GRSP fractions were responsive to marine sediment fertility levels and the understanding of their function in sediment C sequestration will provide new insights into the importance of terrestrial-marine linkages.</div>
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<AbstractText>Glomalin-related soil protein (GRSP), a particular terrigenous-derived carbon (C), is transported to the coastal oceans, where it accumulates in sediments. We hypothesized that terrigenous C (GRSP) accumulation could enhance marine C sequestration, and sediment fertility would increase the C stock in the marine ecosystem. In this study, we tested GRSP contribution to marine sediment C, nitrogen (N) and iron (Fe), and explored whether GRSP deposition varied with sediment fertility levels in the Old Yellow River delta. The mean concentration of total GRSP was 1.10±0.04mgg
<sup>-1</sup>
(0.24MgCha
<sup>-1</sup>
), accounting for 6.41±0.17% of total organic C and 3.75±0.13% of total N in the 0-10cm marine sediments, indicating that the coastal marine system is an important sink of GRSP. GRSP also contained 1.46±0.06% Fe (20.7kgFeha
<sup>-1</sup>
), accounting for 0.058±0.003% of total Fe in marine sediments. Meanwhile, Fe-content in GRSP significantly decreased with distance from the shore, indicating that Fe was released with GRSP transfer and thus GRSP was a new natural Fe fertilization in marine environment. Furthermore, GRSP enhanced marine C sequestration by its rapid deposition and Fe contribution. Combined indicators of sediment fertility (factor 1) were significantly positively correlated with GRSP concentrations by Principal Component Analysis. Co-deposited with nutrient elements, GRSP fractions were accumulated more in more fertile sediments but less in less fertile sediments. GRSP, a mixture of co-existent multiple elements, can be used as a nutrient controlled-release agent in the marine ecosystem. GRSP fractions were responsive to marine sediment fertility levels and the understanding of their function in sediment C sequestration will provide new insights into the importance of terrestrial-marine linkages.</AbstractText>
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<QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName>
</MeshHeading>
<MeshHeading>
<DescriptorName UI="D019015" MajorTopicYN="N">Geologic Sediments</DescriptorName>
</MeshHeading>
<MeshHeading>
<DescriptorName UI="D006023" MajorTopicYN="N">Glycoproteins</DescriptorName>
<QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName>
</MeshHeading>
<MeshHeading>
<DescriptorName UI="D007501" MajorTopicYN="N">Iron</DescriptorName>
</MeshHeading>
<MeshHeading>
<DescriptorName UI="D009584" MajorTopicYN="N">Nitrogen</DescriptorName>
</MeshHeading>
<MeshHeading>
<DescriptorName UI="D045483" MajorTopicYN="Y">Rivers</DescriptorName>
</MeshHeading>
<MeshHeading>
<DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName>
</MeshHeading>
</MeshHeadingList>
<KeywordList Owner="NOTNLM">
<Keyword MajorTopicYN="N">Glomalin-related soil protein</Keyword>
<Keyword MajorTopicYN="N">Iron</Keyword>
<Keyword MajorTopicYN="N">Sediment carbon</Keyword>
<Keyword MajorTopicYN="N">Sediment fertility</Keyword>
<Keyword MajorTopicYN="N">Sediment nitrogen</Keyword>
<Keyword MajorTopicYN="N">Terrigenous carbon</Keyword>
</KeywordList>
</MedlineCitation>
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<History>
<PubMedPubDate PubStatus="received">
<Year>2017</Year>
<Month>10</Month>
<Day>09</Day>
</PubMedPubDate>
<PubMedPubDate PubStatus="revised">
<Year>2017</Year>
<Month>12</Month>
<Day>25</Day>
</PubMedPubDate>
<PubMedPubDate PubStatus="accepted">
<Year>2017</Year>
<Month>12</Month>
<Day>25</Day>
</PubMedPubDate>
<PubMedPubDate PubStatus="pubmed">
<Year>2018</Year>
<Month>1</Month>
<Day>6</Day>
<Hour>6</Hour>
<Minute>0</Minute>
</PubMedPubDate>
<PubMedPubDate PubStatus="medline">
<Year>2018</Year>
<Month>10</Month>
<Day>12</Day>
<Hour>6</Hour>
<Minute>0</Minute>
</PubMedPubDate>
<PubMedPubDate PubStatus="entrez">
<Year>2018</Year>
<Month>1</Month>
<Day>6</Day>
<Hour>6</Hour>
<Minute>0</Minute>
</PubMedPubDate>
</History>
<PublicationStatus>ppublish</PublicationStatus>
<ArticleIdList>
<ArticleId IdType="pubmed">29304499</ArticleId>
<ArticleId IdType="pii">S0048-9697(17)33736-1</ArticleId>
<ArticleId IdType="doi">10.1016/j.scitotenv.2017.12.303</ArticleId>
</ArticleIdList>
</PubmedData>
</pubmed>
<affiliations>
<list>
<country>
<li>République populaire de Chine</li>
</country>
</list>
<tree>
<country name="République populaire de Chine">
<noRegion>
<name sortKey="Wang, Qiang" sort="Wang, Qiang" uniqKey="Wang Q" first="Qiang" last="Wang">Qiang Wang</name>
</noRegion>
<name sortKey="Chen, Jingyan" sort="Chen, Jingyan" uniqKey="Chen J" first="Jingyan" last="Chen">Jingyan Chen</name>
<name sortKey="Dong, Yunwei" sort="Dong, Yunwei" uniqKey="Dong Y" first="Yunwei" last="Dong">Yunwei Dong</name>
<name sortKey="Hong, Hualong" sort="Hong, Hualong" uniqKey="Hong H" first="Hualong" last="Hong">Hualong Hong</name>
<name sortKey="Li, Junwei" sort="Li, Junwei" uniqKey="Li J" first="Junwei" last="Li">Junwei Li</name>
<name sortKey="Liu, Jingchun" sort="Liu, Jingchun" uniqKey="Liu J" first="Jingchun" last="Liu">Jingchun Liu</name>
<name sortKey="Lu, Haoliang" sort="Lu, Haoliang" uniqKey="Lu H" first="Haoliang" last="Lu">Haoliang Lu</name>
<name sortKey="Yan, Chongling" sort="Yan, Chongling" uniqKey="Yan C" first="Chongling" last="Yan">Chongling Yan</name>
</country>
</tree>
</affiliations>
</record>

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