Phanerozoic Record of Global Sea-Level Change
We review Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 ± 50 meters during the Cretaceous, implying that ocean-crust production rates were much...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 2005-11, Vol.310 (5752), p.1293-1298 |
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| container_title | Science (American Association for the Advancement of Science) |
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| creator | Miller, Kenneth G Kominz, Michelle A Browning, James V Wright, James D Mountain, Gregory S Katz, Miriam E Sugarman, Peter J Cramer, Benjamin S Christie-Blick, Nicholas Pekar, Stephen F |
| description | We review Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 ± 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10⁴- to 10⁶-year scale, but a link between oxygen isotope and sea level on the 10⁷-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. Over the past 100 My, sea-level changes reflect global climate evolution from a time of ephemeral Antarctic ice sheets (100 to 33 Ma), through a time of large ice sheets primarily in Antarctica (33 to 2.5 Ma), to a world with large Antarctic and large, variable Northern Hemisphere ice sheets (2.5 Ma to the present). |
| doi_str_mv | 10.1126/science.1116412 |
| format | Article |
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Long-term sea level peaked at 100 ± 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10⁴- to 10⁶-year scale, but a link between oxygen isotope and sea level on the 10⁷-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. 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Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 ± 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10⁴- to 10⁶-year scale, but a link between oxygen isotope and sea level on the 10⁷-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. Over the past 100 My, sea-level changes reflect global climate evolution from a time of ephemeral Antarctic ice sheets (100 to 33 Ma), through a time of large ice sheets primarily in Antarctica (33 to 2.5 Ma), to a world with large Antarctic and large, variable Northern Hemisphere ice sheets (2.5 Ma to the present).</abstract><cop>Washington, DC</cop><pub>American Association for the Advancement of Science</pub><pmid>16311326</pmid><doi>10.1126/science.1116412</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record> |
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| ispartof | Science (American Association for the Advancement of Science), 2005-11, Vol.310 (5752), p.1293-1298 |
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| language | eng |
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| source | American Association for the Advancement of Science; Jstor Complete Legacy |
| subjects | Analysis Canals, Interoceanic Climate change Company growth Cooling Drilling Earth sciences Earth, ocean, space Exact sciences and technology Geologic ages Geology Ice Ice sheets Interoceanic canals Marine Marine geology Oceanography Oceans Organic Chemistry Paleoclimatology Plate Tectonics Review Sea level Sea water Stratigraphy Subsidence Water Water circulation |
| title | Phanerozoic Record of Global Sea-Level Change |
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