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Ventilation record of cold-water corals from Mauritania over the last 30.000 ...
Combined 230ThU and 14C ages in cold-water corals allow accurate reconstruction of ventilation in the past. Here we present a ventilation record of cold-water corals from... -
Core top chlorophyll concentration compared to modern observations in the eas...
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230Th/U-datings from speleothem DH_Kn5 from Dechencave, Germany
We combined central European speleothem growth phases in one stack. The stack includes speleothem growth phases that were compiled from literature as well as three speleothems... -
Speleothem stack from central and western European cave systems
Speleothem growth phases from central European cave systems with ages between 136700 and 56 years before the year 2000 [yr b2k] were stacked and are shown on the age scale [yr... -
230Th/U-datings from speleothem DH_Kn7 from Dechencave, Germany
We combined central European speleothem growth phases in one stack. The stack includes speleothem growth phases that were compiled from literature as well as three speleothems... -
230Th/U-datings from speleothem DH_Kn6 from Dechencave, Germany
We combined central European speleothem growth phases in one stack. The stack includes speleothem growth phases that were compiled from literature as well as three speleothems... -
Uranium-thorium dating of Atlantic cold-water corals from the last 32,000 years
Uranium-thorium dating offers the possibility of absolute age determination of cold-water corals (CWCs). We present here the complementary dataset to "Radiocarbon dating of... -
Cold-water coral Atlantic thermocline ventilation records over the last 32,00...
The radiocarbon analysis of uranium-thorium-dated cold-water corals (CWCs) provides an excellent opportunity for qualitative reconstruction of past ocean circulation and water... -
Radiocarbon dating of Atlantic cold-water corals over the last 32,000 years
The radiocarbon analysis of uranium-thorium-dated cold-water corals (CWCs) provides an excellent opportunity for qualitative reconstruction of past ocean circulation and water...
