The phanerozoic record of global sea-level change

Publication Type  Journal Article
Year of Publication  2005
Authors  Miller, K. G.; Kominz, M. A.; Browning, J. V.; Wright, J. D.; Mountain, G. S.; Katz, M. E.; Sugarman, P. J.; Cramer, B. S.; Christie-Blick, N.; Pekar, S. F.
Journal Title  Science
Volume  310
Issue  5752
Pages  1293-1298
Journal Date  Nov 25
ISBN Number  0036-8075
Accession Number  ISI:000233600200031
Key Words  new-jersey; russian platform; north-atlantic; coastal-plain; time-scale; sequences; stratigraphy; oligocene; events; earth
Abstract  

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 10(4)- to 10(6)-year scale, but a link between oxygen isotope and sea level on the 10(7)-year scale must be due to temperature changes that we attribute to tectonicaliy 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).

Notes  

988KNTimes Cited:78Cited References Count:65

URL  <Go to ISI>://000233600200031
DOI  DOI 10.1126/science.1116412