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Geochemistry of sediment core PG1111
This dataset has no description
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Geochemistry of surface sediment samples from the Bunger Oasis, Antarctica
This dataset has no description
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Geochemistry of sediment core PG1158
This dataset has no description
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Multiproxy dataset from Lake Bolshoe Toko, Siberia (PG2208)
We conducted field work at Lake Bolshoe Toko in the first week of April 2013 as part of the expedition “Yakutia 2013” as a joint campaign of the North Eastern Federal State... -
Plio-Pleistocene Biomarker and Pollen Dataset from IODP Site 361-U1478
Biomarker and pollen data for IODP Site U1478 spanning the Plio-Pleistocene (4 to 1.8 Ma). Organic geochemical data includes the hydrogen isotopic composition of leaf waxes... -
Climate-induced variability in Mediterranean Outflow to the North Atlantic Oc...
Mediterranean Outflow Water (MOW) adds salt and density to open ocean intermediate waters and is therefore an important motor of Atlantic meridional overturning circulation... -
Nannofossil abundance from IODP site 361-U1476 (2.85-1.85 Ma)
A detailed paleoenvironment reconstruction from the Mozambique Channel, western Indian Ocean, based on the calcareous nannoplankton assemblages was conducted for the interval... -
Last glacial period lake sediment data from Lake Sihailongwan, N.E. China
Lake Sihailongwan in Jilin province, NE China, provides the first continuous and almost entirely seasonally laminated sediment record on the East Asian mainland comprising the... -
Mediterranean Outflow Water variability during the Early Pleistocene
Gaining insights into the evolution of Mediterranean Outflow Water (MOW) during the Early Pleistocene climate transition has been so far hampered by the lack of available... -
Varved sediment record from Etoliko Lagoon
To achieve deeper understanding of climate variability during the last millennium in SE Europe, we report new sedimentological and paleoecological data from Etoliko Lagoon,... -
Sea surface temperature variability in the central-western Mediterranean Sea
This study presents the reconstructed evolution of sea surface conditions in the central-western Mediterranean Sea during the late Holocene (2700 years) from a set of... -
Lake Tiefer See varve microfacies, bulk geochemistry, µ-XRF, vegetation openn...
The Holocene sediment record of Lake Tiefer See exhibits striking alternations between well-varved and non-varved intervals. Here we present a high resolution multi-proxy record... -
Stable isotope and Mg/Ca record of IODP Site 339-U1385
Although millennial-scale climate variability (<10 ka) has been well studied during the last glacial cycles, little is known about this important aspect of climate in the... -
Geochemistry, grain sizes and radiocarbon age of sediment core Lz1005 from Am...
The clay mineralogical composition of a 552 cm long sediment core from Lake Terrasovoje in Amery Oasis, East Antarctica, was analysed and compared with that in surface sediments... -
Stable isotope record, carbonate and organic carbon content of the Miocene se...
The Miocene Climatic Optimum (~17-14.7 Ma) represents one of several major interruptions in the long-term cooling trend of the past 50 million years. To date, the processes... -
Separating ITCZ- and ENSO-related rainfall changes in the Galápagos over the ...
We present a 3000-yr rainfall reconstruction from the Galápagos Islands that is based on paired biomarker records from the sediment of El Junco Lake. Located in the eastern... -
North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record
Heinrich events are well documented for the last glaciation, but little is known about their occurrence in older glacial periods of the Pleistocene. Here we report scanning XRF... -
Biogenic sedimentation of DSDP Site 85-574
The equatorial Pacific is an important part of the global carbon cycle and has been affected by climate change through the Cenozoic (65 Ma to present). We present a Miocene... -
Stable isotope record, opal accumulation rate and geochemistry of middle Mioc...
During the middle Miocene, Earth's climate transitioned from a relatively warm phase (Miocene climatic optimum) into a colder mode with re-establishment of permanent ice sheets... -
Linear sedimentation rates and approximate mass accumulation rates at DSDP Si...
A 560-meter-thick sequence of Cenomanian through Pleistocene sediments cored at DSDP Site 462 in the Nauru Basin overlies a 500-meter-thick complex unit of altered basalt flows,...