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Eocene cooling linked to early flow across the Tasmanian Gateway
The warmest global temperatures of the past 85 million years occurred during a prolonged greenhouse episode known as the Early Eocene Climatic Optimum (52-50 Ma). The Early... -
Sporomorphs and quantitative analysis of the Eocene record from IODP Hole 318...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was characterized by an expansion of near-tropical vegetation belts into the... -
Pollen and spores, calculated temperature and precipitation of IODP Hole 318-...
The warmest global climates of the past 65 million years occurred during the early Eocene epoch (about 55 to 48 million years ago), when the Equator-to-pole temperature... -
Palynology and sea surface temperature reconstruction for the mid-Cretaceous ...
The mid-Cretaceous is thought to be a greenhouse world with significantly higher atmospheric pCO2 and sea-surface temperatures as well as a much flatter latitudinal thermal... -
Lower Albian benthic foraminifera
The Early Albian Oceanic Anoxic Event 1b (OAE 1b) black shale is interrupted by one or more ventilation events that display significant changes in benthic and planktic... -
Late Glacial and Holocene palynological data from Füramoos, Southwestern Germany
Palynological data from the Late Glacial and Holocene (c. 14500 – 200 yrs cal. BP) obtained from an ombrotrophic peat bog at Füramoos (southern Germany). -
Dinoflagellate abundances in sediments of Lake Vouliagmeni, Greece
A total of 36 palynological samples, were prepared using standard palynological techniques including freeze-drying, weighing, spiking with Lycopodium spores (Batch Nr. 3140)... -
Late Albian Col de Palluel (SE France, Niveau Breistroffer): results from pla...
This dataset has no description
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Late Glacial and Holocene lead XRF core scanning data from Füramoos, Southwes...
Lead content was analyzed by X-ray fluorescence core scanning (XRF-CS) in samples from the Late Glacial and Holocene (c. 14500 – 200 yrs cal. BP) obtained from an ombrotrophic... -
Late Glacial and Holocene lead isotopes and lead concentration data from Füra...
Lead concentration and stable isotopes were analysed using inductively coupled plasma mass spectrometry (ICP-MS) in samples from an ombrotrophic peat bog at Füramoos (southern... -
(Fig. DR4) 231Pa/230Th record of sediment core MD95-2037
Original data from Guihou et al. (2011) on the revised age model -
(Fig. DR4) Sea surface temperature reconstruction for sediment core MD95-2037
Original data from Calvo et al. 2001 on the revised age model -
(Fig. DR4) Stable oxygen isotope record of Globigerina bulloides of sediment ...
Original data from Calvo et al. 2001 on the revised age model -
(Fig. DR4) Revised age model for Marine Isotope Stage 5 in sediment core MD95...
Based on tuning planktonic d18O data from Calvo et al. (2001) to the planktonic d18O record of MD01-2444 -
(Table S5) Geochemistry of sediment core CIROS-1
This dataset has no description
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(Table S4) Geochemistry of McMurdo Erratic D1
CaO* refers to CaO in the silicate fraction. -
(Table S1) Geochemistry of Cape Roberts Project sediment cores CRP-1, CRP-2, ...
CaO* refers to CaO in the silicate fraction. -
(Table A4) Age tie points for CIROS-1 drillhole
Age tie points for CIROS-1 drillhole according to Harwood et al. [1989], Rieck [1989] and Wilson et al. [1998] and converted to Gradstein et al. [2004] -
(Table A3) Age tie points for Cape Roberts Project (CRP) drillholes, sediment...
Age tie points for Cape Roberts Project (CRP) drillhole according to Gradstein et al. [2004] -
Total organic carbon (TOC) concentration from drillhole FB2001 located in Mes...
We analyzed 10 samples from the FB2001 depth interval 10-9 m for their Total Organic Carbon (TOC) content. This new data set is supplementary to the existing TOC record of...
