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Late Pleistocene planktonic foraminifera of Hole 302-M0004C (Addendum 1)
Data of 302-M0004C-3H-3,18-20 to 302-M0004C-6X-1,96-98 have been produced at the USGS National Center, Reston (VA) -
Physical properties of Hole 302-M0004B
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Physical properties of Hole 302-M0004A
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Physical properties of Hole 302-M0003A
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Physical properties of Hole 302-M0004C
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Age determination and stable carbon isotope ratios of Neogloboquadrina pachyd...
The Integrated Ocean Drilling Program (IODP) Arctic Coring Expedition (ACEX) Hole 4C from the Lomonosov Ridge in the central Arctic Ocean recovered a continuous 18 m record of... -
Reconstruction of continental mean air temperature across the PETM of IODP Ho...
The Palaeocene-Eocene Thermal Maximum (PETM; ~55.5 Ma) is a geologically relatively brief episode of extreme warmth. Both deep and surface ocean temperatures increased by up to... -
Light reflectance (RGB) of Hole 302-M0004C
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Light reflectance (RGB) of Hole 302-M0004B
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Stable carbon isotope ratios of alkane of IODP Hole 302-M0004A
The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming approx ~55 million years ago, superimposed on an already warm world (Zachos et al.,... -
(Table 1) Elemental mean values of the upper Paleocene and lower Eocene in IO...
We reconstruct the latest Paleocene and early Eocene (~57-50 Ma) environmental trends in the Arctic Ocean and focus on the Paleocene-Eocene thermal maximum (PETM) (~55 Ma),... -
Planktonic foraminifera and microfossil composition of IODP Hole 302-M0004C
Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most... -
(Table 1) Geochemistry of the ETM-2 section from IODP Hole 302-M0004A
During the early Eocene, a series of short-term global warming events ("hyperthermals”) occurred in response to the rapid release of carbon into the oceans and atmosphere. In... -
Stable carbon isotope values of TOC and biphytanes for three PETM sections in...
The Paleocene-Eocene Thermal Maximum (PETM; ~56 Ma) and Eocene Thermal Maximum 2 (ETM2; ~53 Ma) are geological short (<200,000 years) episodes of extreme global warming and... -
Chemical composition of Eocene sediments of Hole 302-M0002A
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Chemical composition of Eocene sediments of Hole 302-M0004A
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Sum peak hight and area intensities of bulk X-ray diffraction data of Hole 30...
Depth is given in meter composite depth (mcd) ! -
Relative mineral abundances from bulk fraction X-ray diffraction data of Hole...
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Relative mineral abundances from bulk fraction X-ray diffraction data of Hole...
This dataset has no description
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Relative mineral abundances from bulk fraction X-ray diffraction data of Hole...
This dataset has no description