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Palynological data from cores SG-1 and SG-1b from the Qaidam Basin (Tibetan P...
To reconstruct the timing and underlying forcing of major shifts in the composition of terrestrial ecosystems in arid Central Asia during the late Cenozoic (past ~7 Ma), we... -
Abundance of benthic foraminifera in the late Oligocene-Neogene in ODP Hole 1...
This dataset has no description
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Abundance of benthic foraminifera in the late Oligocene-Neogene in ODP Hole 1...
This dataset has no description
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Abundance of benthic foraminifera in the late Oligocene-Neogene in ODP Hole 1...
This dataset has no description
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Coarse and small fraction carbonate content and accumulation rate from Miocen...
Coarse and small fraction carbonate content and accumulation rate from Miocene to Quaternary, at site 927. The table contains the quantity of less than 32 µm sediment on the... -
Carbonate scenarios analysis from different sources of Fluid inclusions, CCD ...
Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions. -
Carbonate scenarios analysis from different sources of Fluid inclusions, CCD ...
Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions. -
Carbonate scenarios analysis from different sources of Fluid inclusions, CCD ...
Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions. -
Boron isotope and Mg/ca ratio of Trilobatus trilobus
This dataset has no description
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Compile early Pleistocene vegetation from globally distributed boreal and bor...
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Records of Neogene ocean carbonate chemistry using the boron isotope pH proxy
Over the course of the Neogene, the Earth underwent profound climatic shifts from the sustained warmth of the middle Miocene to the development of Plio-Pleistocene... -
Compile late Pleistocene vegetation from globally distributed boreal and bord...
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Branched glycerol dialkyl glycerol dialkyl (brGDGT) distributions in Lake Bai...
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Plant wax n-alkanes measured in Baikal Drilling Project core materials
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Dominant biomes and plant functional type affinity scores derived from publis...
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Lake Baikal paleotemperature record derived from the methylation of brGDGTs
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Isoprenoid glycerol dialkyl glycerol dialkyl (iGDGT) distributions in Lake Ba...
An 8.6 million year reconstruction of paleotemperatures and paleovegetation from Lake Baikal, Russia, derived from Baikal Drilling Project core materials. This dataset also... -
Reconstructed global mean surface temperature
Global mean surface temperatures were calculated from latitudinal stacks of sea surface temperature data, weighted by area to generate a mean sea surface temperature, and then... -
A comprehensive compilation of the seismic stratigraphy markers along the Adr...
The Mediterranean Sea is a natural laboratory for addressing questions on the formation and evolution of continental margins and the relationship between surface and deep... -
Abundance of benthic foraminifera in the late Oligocene-Neogene in ODP Holes ...
Count data for most abundant benthic foraminifera in the late Oligocene-Neogene in ODP Holes 752A, 1139A and 1139A Supplement to: Ridha, Dana; Boomer, Ian; Edgar, Kirsty M...
