(Table S1) Stable oxygen isotope record of barite from DSDP Leg 85 sites
| Cobertura |
MEDIAN LATITUDE: 3.318313 * MEDIAN LONGITUDE: -128.916950 * SOUTH-BOUND LATITUDE: 0.498500 * WEST-BOUND LONGITUDE: -135.036000 * NORTH-BOUND LATITUDE: 5.850000 * EAST-BOUND LONGITUDE: -113.842000 * DATE/TIME START: 1982-03-19T00:00:00 * DATE/TIME END: 1982-04-21T00:00:00 * MINIMUM ELEVATION: -4561.0 m * MAXIMUM ELEVATION: -3893.0 m |
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| Data(s) |
30/11/2004
|
| Resumo |
Oxygen isotopes in marine sulfate (d18O SO4) measured in marine barite show variability over the past 10 million years, including a 5per mil decrease during the Plio-Pleistocene, with near-constant values during the Miocene that are slightly enriched over the modern ocean. A numerical model suggests that sea level fluctuations during Plio-Pleistocene glacial cycles affected the sulfur cycle by reducing the area of continental shelves and increasing the oxidative weathering of pyrite. The data also require that sulfate concentrations were 10 to 20% lower in the late Miocene than today. |
| Formato |
text/tab-separated-values, 477 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.772068 doi:10.1594/PANGAEA.772068 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Turchyn, Alexandra V; Schrag, Daniel P (2004): Oxygen isotope constraints on the sulfur cycle over the past 10 million years. Science, 303(5666), 2004-2007, doi:10.1126/science.1092296 |
| Palavras-Chave | #85-571; 85-572A; 85-573; 85-573A; 85-574; 85-574A; 85-575; 85-575C; AGE; Deep Sea Drilling Project; delta 18O, barite; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Leg85; North Pacific; North Pacific/FLANK; North Pacific/TROUGH; ODP sample designation; Sample code/label; Sample code/label 2 |
| Tipo |
Dataset |
