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Middle Miocene Climate-Carbon Cycle Dynamics: A Key to Understand Future Tren...
Benthic foraminiferal stable isotopes from ODP Sites 1146A/1146C and 1237B/1237C, and IODP sites U1337A/U1337C/U1337D, U1338A-C and U1443A-C with revised downcore depths and... -
Compiled 14C reservoir ages from the northern Northeast Atlantic, Iberian Mar...
Compiled shallow sub-surface radiocarbon 'reservoir ages' from the northern Northeast Atlantic, Iberian Margin and Southern Ocean -
Revised age models and foraminiferal records obtained for the Last Interglaci...
The dataset contains the revised age models and foraminiferal records obtained for the Last Interglacial period in six marine sediment cores: - the Southern Ocean core MD02-2488... -
Phytoplankton carbon biomass in high-nutrient low-chlorophyll subantarctic wa...
This dataset has no description
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Phytoplankton pigment concentration in high-nutrient low-chlorophyll subantar...
This dataset has no description
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Sea surface temperature reconstruction for sediment core KH-10-7 COR1GC from ...
Centennial and millennial scale variability of Southern Ocean temperature is poorly known, due to both short instrumental records and sparsely distributed high-resolution... -
Diatom percentage abundances for sediment core KH-10-7 COR1GC from the Conrad...
Centennial and millennial scale variability of Southern Ocean temperature is poorly known, due to both short instrumental records and sparsely distributed high-resolution... -
Phytoplankton community composition, pigment concentration and CTD measuremen...
The CTD and phytoplankton microscopy and pigment data deposited here were collected during a 3-week voyage on board of the New Zealand R/V Tangaroa to the Campbell Plateau... -
Bulk and diatom-bound nitrogen isotope ratios, opal, TOC, and TN from ODP Hol...
Intense seasonal productivity and carbon drawdown on the West Antarctic Peninsula (WAP) is driven by upwelling of nutrient-rich Circumpolar Deep Water (CDW) and subsequent... -
Downcore depths, ages and benthic foraminiferal stable isotopes (δ¹³C and δ¹⁸...
This dataset has no description
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Downcore depths, ages and benthic foraminiferal stable isotopes (δ¹³C) in sed...
This dataset has no description
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Downcore depths, ages and benthic foraminiferal stable isotopes (δ¹⁸O and δ¹³...
This dataset has no description
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Downcore depths, ages and benthic foraminiferal stable isotopes (δ¹⁸O and δ¹³...
This dataset has no description
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Downcore depths, ages and benthic foraminiferal stable isotopes (δ¹⁸O and δ¹³...
This dataset has no description
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Annotated Southern Ocean diatom LM micrographs from POLARSTERN cruise PS103, ...
Samples were taken during expeditions PS103 by 20 µm mesh size plankton nets from ca. 15 to 0 m depth. To obtain clean siliceous diatom frustules, the samples were oxidized... -
Annotated Southern Ocean diatom LM micrographs from POLARSTERN cruise PS103, ...
Samples were taken during expeditions PS103 by 20 µm mesh size plankton nets from ca. 15 to 0 m depth. To obtain clean siliceous diatom frustules, the samples were oxidized... -
Annotated Southern Ocean diatom LM micrographs from POLARSTERN cruise PS103, ...
Samples were taken during expeditions PS103 by 20 µm mesh size plankton nets from ca. 15 to 0 m depth. To obtain clean siliceous diatom frustules, the samples were oxidized... -
Annotated Southern Ocean diatom LM micrographs from POLARSTERN cruise PS103, ...
Samples were taken during expeditions PS103 by 20 µm mesh size plankton nets from ca. 15 to 0 m depth. To obtain clean siliceous diatom frustules, the samples were oxidized... -
Annotated Southern Ocean diatom LM micrographs from POLARSTERN cruise PS79, 1...
Samples were taken during expeditions ANT-XXVII/2 (PS79) by 20 µm mesh size plankton nets from ca. 15 to 0 m depth. To obtain clean siliceous diatom frustules, the samples were... -
Annotated Southern Ocean diatom LM micrographs from POLARSTERN cruise PS79, 1...
Samples were taken during expeditions ANT-XXVII/2 (PS79) by 20 µm mesh size plankton nets from ca. 15 to 0 m depth. To obtain clean siliceous diatom frustules, the samples were...