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Meteorological records from the Vernagtferner Basin - Vernagtbach station, fo...
This dataset has no description
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Meteorological records from the Vernagtferner Basin - Vernagtbach station, fo...
This dataset has no description
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Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
This dataset has no description
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Depth age model of sediment core MD07-3134
This dataset has no description
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(Table 3) U-series disequilibrium ages measured on Amundsen Sea cold-water co...
Decay constants are 9.1577 x 10-6/yr for 230Th, 2.826 x 10-6/yr for 234U, and 1.55125 x 10-10/yr for 238U. -
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... -
Morphometry of planktonic foraminifera tests from surface sediment samples at...
This dataset has no description
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(Table 1) Age determination of sediment core RAPiD-15-4P
Radiocarbon ages were converted to calendar ages using Calib 5.1 IntCal (Reimer et al., 2004). Years B.P., years before A.D. 1950. By using the assigned stratigraphic age... -
(Table 1) Age comparison between the GPTS and ODP Site 181-1123 age model for...
Today the deep western boundary current (DWBC) east of New Zealand is the most important route for deep water entering the Pacific Ocean. Large-scale changes in deep water... -
Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
(Table 3) Age determination of sediment cores from the SW Pacific Ocean
Eight- to ten-point depth profiles (from 1200 to 4800 m water depth) of oxygen and carbon isotopic values derived from benthic foraminifera, averaged over selected times in the... -
CO2 emission from ant vents (Atta cephalotes) at La Selva Biological Station,...
NOTE: in the file "vent values.xlsx" of doi:10.1594/PANGAEA.887400 there is a brief description of the methodology and the relevance of the start/end points. -
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... -
(Fig. 3c) Difference between measured and calculated settlement of the Omok-S...
This dataset has no description
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(Supplement 3) Monthly mean meteorological buoy measurements in the Iceland S...
This dataset has no description
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(Supplement 2) Daily meteorological buoy measurements in the Iceland Sea 2007...
This dataset has no description
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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... -
Spacing and amplitude of IR temperature anomalies and hydrate content of sedi...
Large uncertainties about the energy resource potential and role in global climate change of gas hydrates result from uncertainty about how much hydrate is contained in marine... -
Heating induced temperature difference measurements from the modular buoy 202...
Temperature and heating-induced temperature differences were measured along a chain of thermistors. 2020M26 (a.k.a. Bruncin IMB042) is an autonomous modular instrument that was... -
Heating induced temperature difference measurements from the modular buoy 202...
Temperature and heating-induced temperature differences were measured along a chain of thermistors. 2020M26 (a.k.a. Bruncin IMB042) is an autonomous modular instrument that was...
