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Carbonate analysis from different GH Expeditions in the Japan Sea
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Uvigerina-based Mg/Ca ratios from different GH Expeditions in the Japan Sea
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Uvigerina-based δ¹⁸O and Mg/Ca ratios from IODP Site 346-U1427 and KR15 in Ja...
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The oxygen isotopic composition of intermediate-to-deep Arctic seawater since...
The oxygen isotopic composition of benthic foraminifera (d18Ob) is widely used to date and correlate marine sediment sequences. However, d18Ob has found comparatively little use... -
Uvigerina-based d18O and Mg/Ca data together with a new Japan Sea core-top Mg...
Glacial isolation of the Japan Sea results in poor carbonate preservation and unusually low oxygen isotope (d18O) ratios from low-saline/low-d18O waters accumulating in the... -
Temperature gradient between IODP Site 306-U1313 and ODP Site 162-982
Temperature gradients listed in this dataset were used to assess the potential connection between upper ocean stratification at IODP Site U1313 (41°N, 33°W) and northward heat... -
Benthic and planktic foraminiferal carbon and oxygen isotopes and Mg/Ca-deriv...
We reconstructed the Indian Monsoon variability of the Earth's strongest hydrological system, at International Ocean Discovery Program (IODP) Expedition 353 Site U1448 in the... -
Planktic foraminiferal (Globigerinoides ruber) oxygen isotopes and Mg/Ca-deri...
We collected a suite of core top samples during R/V Sonne Cruise SO257 in May 2017 along the Western Australian Margin to monitor the variability of Southern Hemisphere tropical... -
Shelf ecosystems along the U.S. Atlantic Coastal Plain prior to and during th...
The Paleocene-Eocene Thermal Maximum (PETM) is the most pronounced climate event of the early Paleogene. It is characterized by negative δ18O and δ13C excursions recorded in... -
Evolution of sea surface hydrology along the Western Australian Margin over t...
We collected a suite of core top samples during R/V Sonne Cruise SO257 in May 2017 along the Western Australian Margin to monitor the variability of Southern Hemisphere tropical... -
Age model, alkenones and stable isotopes of sediment core MSM45-31-1 (MSM45_4...
The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to... -
Planktic foraminiferal (Globigerinoides ruber) oxygen isotopes and Mg/Ca-deri...
We collected a suite of core top samples during R/V Sonne Cruise SO257 in May 2017 along the Western Australian Margin to monitor the variability of Southern Hemisphere tropical... -
Oxygen isotopes, sea surface temperature, and sea surface salinity fom CTD du...
We collected a suite of core top samples during R/V Sonne Cruise SO257 in May 2017 along the Western Australian Margin to monitor the variability of Southern Hemisphere tropical... -
Continous thermosalinograph oceanography during SONNE cruise SO257
We collected a suite of core top samples during R/V Sonne Cruise SO257 in May 2017 along the Western Australian Margin to monitor the variability of Southern Hemisphere tropical... -
Mg/Ca ratios in benthic foraminifera from surface sediments
Today, climate change has become an issue of global significance. These changes are known to be deeply related to heat distribution and paleoceanographic variations. On the... -
Temperature estimates based on Mg/Ca and δ18O for the South Dover Bridge core
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Benthic foraminifera stable isotope ratios in the South Dover Bridge core
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Bulk carbonate stable isotope ratios in the South Dover Bridge core
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Planktic to benthic foraminifera ratio in the South Dover Bridge core
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Kaolinite content in the South Dover Bridge core
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