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Temperature difference after the heating cycle from the sea ice mass balance ...
Temperature and heating-induced temperature were measured along a chain of thermistors. Digital Thermistor Chain DTC33 is an autonomous instrument that was installed on drifting... -
Temperature difference after the heating cycle from the sea ice mass balance ...
Temperature and heating-induced temperature were measured along a chain of thermistors. Digital Thermistor Chain DTC31 is an autonomous instrument that was installed on drifting... -
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
(Table 2c) Planktic and benthic 14C and 14C reservoir ages of sediment core M...
All 14C dates are rounded to decades. Planktic plateau boundaries were either defined at or in between single 14C ages of the records. For reasons of specimen availability... -
Last millennium surface-thermocline temperature difference reconstructions fr...
This data accompanies Hess et al. (2026, Science Advances). It consists of Last Millennium (750 CE to present) surface-thermocline temperature differences from the Indonesian... -
Seawater carbonate chemistry and calcification mechanisms of three Hawaiian c...
Here, we used boron-based geochemical proxies (δ11B, B/Ca) to investigate how three common Hawaiian coral species (Montipora capitata, Porites compressa, Porites lobata)... -
Seawater carbonate chemistry and growth rates, carbon utilization and the int...
Ocean acidification (OA) appears to have diverse impacts on calcareous coccolithophores, but the cellular processes underlying these responses are not well understood. Here we... -
Seawater carbonate chemistry and gastrovascular cavity pH, calcification of M...
Coral polyps have a fluid-filled internal compartment, the gastrovascular cavity (GVC). Respiration and photosynthesis cause large daily excursions in GVC oxygen concentration... -
Seawater carbonate chemistry, clearance rates, respiration rates, condition i...
The decline in ocean water pH and changes in carbonate saturation states through anthropogenically mediated increases in atmospheric CO2 levels may pose a hazard to marine... -
(Table 1) Age determimnation of sediment core MD01-2403
Significantly older 14C ages by 2500-7900 years are found for sedimentary total organic carbon (TOC) when compared to ages of codeposited surface-dwelling foraminifera in the... -
AICC2023, NGRIP
Version 2, 2026-02-05: Previous version doi:10.1594/PANGAEA.961020 contains errors in ice age AICC2012 and gas age AICC2012. -
Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
This dataset has no description
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Phosphorus flux of sediment core Burg17-C
This dataset has no description
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Correlation of sediment cores Burg17-C and Burg17-B
This dataset has no description
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Surface and bottom water reconstructions for ODP Site 177-1094
This dataset has no description
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(Supplement Table S6) Stable isotopes of ODP Site 154-926
This dataset has no description
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Stable oxygen isotope and Mg/Ca ratios of planktonic foraminifera, and SST ca...
Sediment depth is given in mcd. -
Stable oxygen isotope and Mg/Ca ratios of planktonic foraminifera, and SST ca...
Sediment depth is given in mcd. -
(Table 1) Age determination of IODP Hole 323-U1340A
DEPTH, sediment/rock [m] is given in mcd. -
Planktonic and benthic foraminiferal stable isotopes, SSTs and thermocline te...
We present sea surface, upper thermocline, and benthic d18O data, as well as temperature and paleoproductivity proxy data, from the International Marine Global Change Study...
