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Sea surface and subsurface temperature reconstruction for ODP Site 202-1240
Please contact the author Leopoldo Pena lpena@ub.edu to obtain the data. -
Underway fCO2 measurements off NW Africa during POSEIDON cruise POS399 in Jun...
SST was taken from the ship's thermosalinograph (Seabird SBE21 with an external SBE38). Data were only recorded until 17. June. SST data after 17. June were estimated from an... -
Reconstruction of sea surface temperature and export productivity of sediment...
This dataset has no description
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UK`37 and sea surface temperature of Site 177-1089 (Table A-9)
Depth, sediment = composite depth -
SST (warm/cold season, calculated from stable oxygen isotopes) of sediment co...
This dataset has no description
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SST, SSS, SId of core MD95-2009 (LGM)
This dataset has no description
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SST, SSS, SId of core MD95-2010 (LGM)
This dataset has no description
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SST, SSS, SId of core MD95-2002 (LGM)
This dataset has no description
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SST (annual mean, calculated from stable oxygen isotopes) of sediment core MD...
This dataset has no description
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SST data (calculated from UK37 Alkenones) of sediment core MD97-2148
This dataset has no description
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Atlantic sea surface temperatures during the last glacial maximum (LGM) time ...
This dataset has no description
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Deciphering the termination of the Messinian salinity crisis: the alkenone re...
The late Miocene Messinian salinity crisis (MSC; 5.97–5.33 Ma) transformed the Mediterranean basin into the youngest salt giant in Earth history. The paleoenvironment and the... -
Paleointensity, stable oxygen isotopes and sea surface temperature data of tw...
Data include the geomagnetic relative paleointensity, stable oxygen isotope and sea surface temperautre derived from the sediments of the north of South China Sea. Stable oxygen... -
Coherency (ETP) of C37 alkenones mass accumulations rate from IODP Site 321-U...
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of C37 alkenones mass accumulations rate from ODP Site 138-850
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of C37 alkenones mass accumulations rate from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from IODP Site 321-U1338
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from ODP Site 138-850
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of δ13C from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.