Tracking the rise of eukaryotes to ecological dominance with zinc isotopes
The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the ocean. Based on an extensive new sedimentary Zn isotope record across Earth's history, we provide evidence for a fundamental shift in the marine Zn cycle ~800 million years ago. We discuss a wide range of p...
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Published in | Geobiology Vol. 16; no. 4; pp. 341 - 352 |
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Main Authors | , , , , , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
England
Wiley Subscription Services, Inc
01.07.2018
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ISSN | 1472-4677 1472-4669 1472-4669 |
DOI | 10.1111/gbi.12289 |
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Abstract | The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the ocean. Based on an extensive new sedimentary Zn isotope record across Earth's history, we provide evidence for a fundamental shift in the marine Zn cycle ~800 million years ago. We discuss a wide range of potential drivers for this transition and propose that, within available constraints, a restructuring of marine ecosystems is the most parsimonious explanation for this shift. Using a global isotope mass balance approach, we show that a change in the organic Zn/C ratio is required to account for observed Zn isotope trends through time. Given the higher affinity of eukaryotes for Zn relative to prokaryotes, we suggest that a shift toward a more eukaryote‐rich ecosystem could have provided a means of more efficiently sequestering organic‐derived Zn. Despite the much earlier appearance of eukaryotes in the microfossil record (~1700 to 1600 million years ago), our data suggest a delayed rise to ecological prominence during the Neoproterozoic, consistent with the currently accepted organic biomarker records. |
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AbstractList | The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the ocean. Based on an extensive new sedimentary Zn isotope record across Earth's history, we provide evidence for a fundamental shift in the marine Zn cycle ~800 million years ago. We discuss a wide range of potential drivers for this transition and propose that, within available constraints, a restructuring of marine ecosystems is the most parsimonious explanation for this shift. Using a global isotope mass balance approach, we show that a change in the organic Zn/C ratio is required to account for observed Zn isotope trends through time. Given the higher affinity of eukaryotes for Zn relative to prokaryotes, we suggest that a shift toward a more eukaryote‐rich ecosystem could have provided a means of more efficiently sequestering organic‐derived Zn. Despite the much earlier appearance of eukaryotes in the microfossil record (~1700 to 1600 million years ago), our data suggest a delayed rise to ecological prominence during the Neoproterozoic, consistent with the currently accepted organic biomarker records. The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the ocean. Based on an extensive new sedimentary Zn isotope record across Earth's history, we provide evidence for a fundamental shift in the marine Zn cycle ~800 million years ago. We discuss a wide range of potential drivers for this transition and propose that, within available constraints, a restructuring of marine ecosystems is the most parsimonious explanation for this shift. Using a global isotope mass balance approach, we show that a change in the organic Zn/C ratio is required to account for observed Zn isotope trends through time. Given the higher affinity of eukaryotes for Zn relative to prokaryotes, we suggest that a shift toward a more eukaryote-rich ecosystem could have provided a means of more efficiently sequestering organic-derived Zn. Despite the much earlier appearance of eukaryotes in the microfossil record (~1700 to 1600 million years ago), our data suggest a delayed rise to ecological prominence during the Neoproterozoic, consistent with the currently accepted organic biomarker records.The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the ocean. Based on an extensive new sedimentary Zn isotope record across Earth's history, we provide evidence for a fundamental shift in the marine Zn cycle ~800 million years ago. We discuss a wide range of potential drivers for this transition and propose that, within available constraints, a restructuring of marine ecosystems is the most parsimonious explanation for this shift. Using a global isotope mass balance approach, we show that a change in the organic Zn/C ratio is required to account for observed Zn isotope trends through time. Given the higher affinity of eukaryotes for Zn relative to prokaryotes, we suggest that a shift toward a more eukaryote-rich ecosystem could have provided a means of more efficiently sequestering organic-derived Zn. Despite the much earlier appearance of eukaryotes in the microfossil record (~1700 to 1600 million years ago), our data suggest a delayed rise to ecological prominence during the Neoproterozoic, consistent with the currently accepted organic biomarker records. |
Author | Owens, Jeremy Zhao, Ming‐Yu Zumberge, Alex J. Isson, Terry T. Gueguen, Bleuenn Rainbird, Robert H. Konhauser, Kurt O. Lyons, Timothy W. Reinhard, Christopher T. Planavsky, Noah J. Rooney, Alan D. Stueeken, Eva E. John, Seth G. Love, Gordon D. Asael, Dan McCrow, John Dupont, Christopher L. Gill, Ben C. |
Author_xml | – sequence: 1 givenname: Terry T. orcidid: 0000-0002-1040-0230 surname: Isson fullname: Isson, Terry T. email: terry.t.isson@gmail.com organization: Yale University – sequence: 2 givenname: Gordon D. surname: Love fullname: Love, Gordon D. organization: University of California, Riverside – sequence: 3 givenname: Christopher L. surname: Dupont fullname: Dupont, Christopher L. organization: J. Craig Venter Institute – sequence: 4 givenname: Christopher T. surname: Reinhard fullname: Reinhard, Christopher T. organization: Georgia Institute of Technology – sequence: 5 givenname: Alex J. surname: Zumberge fullname: Zumberge, Alex J. organization: University of California, Riverside – sequence: 6 givenname: Dan surname: Asael fullname: Asael, Dan organization: Yale University – sequence: 7 givenname: Bleuenn surname: Gueguen fullname: Gueguen, Bleuenn organization: Université de Bretagne Occidentale – sequence: 8 givenname: John surname: McCrow fullname: McCrow, John organization: J. Craig Venter Institute – sequence: 9 givenname: Ben C. surname: Gill fullname: Gill, Ben C. organization: Virginia Tech – sequence: 10 givenname: Jeremy surname: Owens fullname: Owens, Jeremy organization: Florida State University – sequence: 11 givenname: Robert H. surname: Rainbird fullname: Rainbird, Robert H. organization: Geological Survey of Canada – sequence: 12 givenname: Alan D. orcidid: 0000-0002-5023-2606 surname: Rooney fullname: Rooney, Alan D. organization: Yale University – sequence: 13 givenname: Ming‐Yu surname: Zhao fullname: Zhao, Ming‐Yu organization: Yale University – sequence: 14 givenname: Eva E. orcidid: 0000-0001-6861-2490 surname: Stueeken fullname: Stueeken, Eva E. organization: University of St Andrews, St Andrews – sequence: 15 givenname: Kurt O. surname: Konhauser fullname: Konhauser, Kurt O. organization: University of Alberta – sequence: 16 givenname: Seth G. surname: John fullname: John, Seth G. organization: University of Southern Carolina – sequence: 17 givenname: Timothy W. surname: Lyons fullname: Lyons, Timothy W. organization: University of California, Riverside – sequence: 18 givenname: Noah J. surname: Planavsky fullname: Planavsky, Noah J. organization: Yale University |
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Keywords | eukaryotes ocean chemistry marine productivity zinc isotopes carbon cycle zinc Earth history |
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Snippet | The biogeochemical cycling of zinc (Zn) is intimately coupled with organic carbon in the ocean. Based on an extensive new sedimentary Zn isotope record across... |
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SubjectTerms | Biogeochemical cycles Biogeochemistry Biomarkers carbon cycle Earth Earth history Ecosystems Eukaryota Eukaryotes Fossils Isotopes Marine ecosystems marine productivity ocean chemistry Organic carbon Prokaryotes Tracking Zinc Zinc isotopes |
Title | Tracking the rise of eukaryotes to ecological dominance with zinc isotopes |
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