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Chemical composition of Eocene sediments of Hole 302-M0002A
This dataset has no description
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Analysis of organic carbon from Hole 302-M0004C
This dataset has no description
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Analysis of organic carbon from Hole 302-M0004B
This dataset has no description
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Analysis of organic carbon from Hole 302-M0004A
This dataset has no description
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Analysis of organic carbon from Hole 302-M0002A
This dataset has no description
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Bulk organic geochemistry of Hole 302-M0004A
Comment on sulfur values: The high sulfur values > 5% determined with the LECO instrument are minimum values as shown by re-measurements using an ELTRA-CS 500 instrument... -
Bulk organic geochemistry of Hole 302-M0004B
Comment on sulfur values: The high sulfur values > 5% determined with the LECO instrument are minimum values as shown by re-measurements using an ELTRA-CS 500 instrument... -
Bulk organic geochemistry of Hole 302-M0002A
Comment on sulfur values: The high sulfur values > 5% determined with the LECO instrument are minimum values as shown by re-measurements using an ELTRA-CS 500 instrument... -
Carbonate geochemistry of IODP Hole 302-M0004A
This dataset belongs to a data compilation that contains total organic carbon content, calcium carbonate content and concentrations for major elements, covering the... -
Major element composition of IODP Hole 302-M0004A
This dataset belongs to a data compilation that contains total organic carbon content, calcium carbonate content and concentrations for major elements, covering the... -
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... -
(Table 1) Nd-Hf isotopes from leachates and detrital materials of the Arctic ...
The warm and saline North Atlantic inflow to the Arctic Ocean is a major component of high northern latitude circulation and the main mechanism of deep water renewal in the... -
(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... -
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 2) Geochemical analysis from IODP Exp302
Geochemical analyses of biogenic opal, total organic carbon (TOC), total sulfur (TS), and stable sulfur isotopic composition were conducted on the middle Eocene section of the... -
(Appendix A) Geochemistry for Units 1/6, 2, and the upper part of Unit 3 of I...
Integrated Ocean Drilling Program (IODP) Expedition 302 Arctic Coring Expedition (ACEX) obtained the first relatively continuous long sediment cores from the Lomonosov Ridge in... -
Geochemistry and P and Fe fractionation in anoxic sediments
We investigated the phosphorus (P) and iron (Fe) fractionation in four cores with anoxic sediments, deposited during the mid-Cretaceous oceanic anoxic event 2 (~94 Ma) and the... -
(Table S1) Palynology of IODP Hole 302-M0004A
The Palaeocene/Eocene thermal maximum, 55 million years ago, was a brief period of widespread, extreme climatic warming (Zachos et al., 2003; Kennett and Stott, 1991,... -
(Table 1) The 10Be and 9Be isotope record of IODP EXP202 composite Site
The upper 200 m of the sediments recovered during IODP Leg 302, the Arctic Coring Expedition (ACEX), to the Lomonosov Ridge in the central Arctic Ocean consist almost... -
(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),...
