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Coastal El Niño triggers rapid marine silicate alteration on the seafloor
Marine silicate alteration plays a key role in the global carbon and cation cycles, although the timeframe of this process in response to extreme weather events is poorly understood. Here we investigate surface sediments across the Peruvian margin before and after extreme rainfall and runoff (coasta...
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| Published in: | Nature communications 2023-03, Vol.14 (1), p.1676-1676, Article 1676 |
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| creator | Geilert, Sonja Frick, Daniel A. Garbe-Schönberg, Dieter Scholz, Florian Sommer, Stefan Grasse, Patricia Vogt, Christoph Dale, Andrew W. |
| description | Marine silicate alteration plays a key role in the global carbon and cation cycles, although the timeframe of this process in response to extreme weather events is poorly understood. Here we investigate surface sediments across the Peruvian margin before and after extreme rainfall and runoff (coastal El Niño) using Ge/Si ratios and laser-ablated solid and pore fluid Si isotopes (δ
30
Si). Pore fluids following the rainfall show elevated Ge/Si ratios (2.87 µmol mol
−1
) and δ
30
Si values (3.72‰), which we relate to rapid authigenic clay formation from reactive terrigenous minerals delivered by continental runoff. This study highlights the direct coupling of terrestrial erosion and associated marine sedimentary processes. We show that marine silicate alteration can be rapid and highly dynamic in response to local weather conditions, with a potential impact on marine alkalinity and CO
2
-cycling on short timescales of weeks to months, and thus element turnover on human time scales.
This study identifies the rapidness of marine mineral reactions, directly after an extreme rainfall event. The reactions have the potential to affect marine cation and CO
2
cycling, impacting element turnover on human time scales |
| doi_str_mv | 10.1038/s41467-023-37186-5 |
| format | article |
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30
Si). Pore fluids following the rainfall show elevated Ge/Si ratios (2.87 µmol mol
−1
) and δ
30
Si values (3.72‰), which we relate to rapid authigenic clay formation from reactive terrigenous minerals delivered by continental runoff. This study highlights the direct coupling of terrestrial erosion and associated marine sedimentary processes. We show that marine silicate alteration can be rapid and highly dynamic in response to local weather conditions, with a potential impact on marine alkalinity and CO
2
-cycling on short timescales of weeks to months, and thus element turnover on human time scales.
This study identifies the rapidness of marine mineral reactions, directly after an extreme rainfall event. The reactions have the potential to affect marine cation and CO
2
cycling, impacting element turnover on human time scales</description><identifier>ISSN: 2041-1723</identifier><identifier>EISSN: 2041-1723</identifier><identifier>DOI: 10.1038/s41467-023-37186-5</identifier><identifier>PMID: 36966137</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>140/125 ; 140/58 ; 147/28 ; 704/106/829/827 ; 704/47/4112 ; 704/47/4113 ; Ablation ; Alkalinity ; Carbon cycle ; Carbon dioxide ; Cations ; Clay minerals ; Cycles ; El Nino ; Extreme weather ; Germanium ; Humanities and Social Sciences ; Isotopes ; multidisciplinary ; Ocean floor ; Rain ; Rainfall ; Runoff ; Science ; Science (multidisciplinary) ; Sediments ; Silicon isotopes ; Time ; Weather</subject><ispartof>Nature communications, 2023-03, Vol.14 (1), p.1676-1676, Article 1676</ispartof><rights>The Author(s) 2023</rights><rights>2023. The Author(s).</rights><rights>The Author(s) 2023. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c541t-590029eba0006a84fd89e0fa16d3ab97be889898d61f34955f0fee5db65b0c3f3</citedby><cites>FETCH-LOGICAL-c541t-590029eba0006a84fd89e0fa16d3ab97be889898d61f34955f0fee5db65b0c3f3</cites><orcidid>0000-0002-4186-5997 ; 0000-0002-8530-3064 ; 0000-0001-8653-0448 ; 0000-0002-8971-5867 ; 0000-0002-1745-4418</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2790695314/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2790695314?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,885,25753,27924,27925,37012,37013,44590,53791,53793,75126</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/36966137$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Geilert, Sonja</creatorcontrib><creatorcontrib>Frick, Daniel A.</creatorcontrib><creatorcontrib>Garbe-Schönberg, Dieter</creatorcontrib><creatorcontrib>Scholz, Florian</creatorcontrib><creatorcontrib>Sommer, Stefan</creatorcontrib><creatorcontrib>Grasse, Patricia</creatorcontrib><creatorcontrib>Vogt, Christoph</creatorcontrib><creatorcontrib>Dale, Andrew W.</creatorcontrib><title>Coastal El Niño triggers rapid marine silicate alteration on the seafloor</title><title>Nature communications</title><addtitle>Nat Commun</addtitle><addtitle>Nat Commun</addtitle><description>Marine silicate alteration plays a key role in the global carbon and cation cycles, although the timeframe of this process in response to extreme weather events is poorly understood. Here we investigate surface sediments across the Peruvian margin before and after extreme rainfall and runoff (coastal El Niño) using Ge/Si ratios and laser-ablated solid and pore fluid Si isotopes (δ
30
Si). Pore fluids following the rainfall show elevated Ge/Si ratios (2.87 µmol mol
−1
) and δ
30
Si values (3.72‰), which we relate to rapid authigenic clay formation from reactive terrigenous minerals delivered by continental runoff. This study highlights the direct coupling of terrestrial erosion and associated marine sedimentary processes. We show that marine silicate alteration can be rapid and highly dynamic in response to local weather conditions, with a potential impact on marine alkalinity and CO
2
-cycling on short timescales of weeks to months, and thus element turnover on human time scales.
This study identifies the rapidness of marine mineral reactions, directly after an extreme rainfall event. The reactions have the potential to affect marine cation and CO
2
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Commun</addtitle><date>2023-03-25</date><risdate>2023</risdate><volume>14</volume><issue>1</issue><spage>1676</spage><epage>1676</epage><pages>1676-1676</pages><artnum>1676</artnum><issn>2041-1723</issn><eissn>2041-1723</eissn><abstract>Marine silicate alteration plays a key role in the global carbon and cation cycles, although the timeframe of this process in response to extreme weather events is poorly understood. Here we investigate surface sediments across the Peruvian margin before and after extreme rainfall and runoff (coastal El Niño) using Ge/Si ratios and laser-ablated solid and pore fluid Si isotopes (δ
30
Si). Pore fluids following the rainfall show elevated Ge/Si ratios (2.87 µmol mol
−1
) and δ
30
Si values (3.72‰), which we relate to rapid authigenic clay formation from reactive terrigenous minerals delivered by continental runoff. This study highlights the direct coupling of terrestrial erosion and associated marine sedimentary processes. We show that marine silicate alteration can be rapid and highly dynamic in response to local weather conditions, with a potential impact on marine alkalinity and CO
2
-cycling on short timescales of weeks to months, and thus element turnover on human time scales.
This study identifies the rapidness of marine mineral reactions, directly after an extreme rainfall event. The reactions have the potential to affect marine cation and CO
2
cycling, impacting element turnover on human time scales</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>36966137</pmid><doi>10.1038/s41467-023-37186-5</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-4186-5997</orcidid><orcidid>https://orcid.org/0000-0002-8530-3064</orcidid><orcidid>https://orcid.org/0000-0001-8653-0448</orcidid><orcidid>https://orcid.org/0000-0002-8971-5867</orcidid><orcidid>https://orcid.org/0000-0002-1745-4418</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | 140/125 140/58 147/28 704/106/829/827 704/47/4112 704/47/4113 Ablation Alkalinity Carbon cycle Carbon dioxide Cations Clay minerals Cycles El Nino Extreme weather Germanium Humanities and Social Sciences Isotopes multidisciplinary Ocean floor Rain Rainfall Runoff Science Science (multidisciplinary) Sediments Silicon isotopes Time Weather |
| title | Coastal El Niño triggers rapid marine silicate alteration on the seafloor |
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