-
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... -
Paleomagnetic analysis of the Oligocene to early Miocene sediments of IODP SI...
Fine-grained magnetic particles in deep-sea sediments often statistically align with the ambient magnetic field during (and shortly after) deposition and can therefore record... -
Volcanic ash layer description and thickness analysis from different DSDP, OD...
Ocean drilling provides a global record of deposits throughout the oceans. An international collaborative ocean research programme was established in 1966, and the International... -
Calcium isotope ratios from marine barite and carbonate over Paleocene-Eocene...
Carbonates are invaluable archives of the past, and have been used extensively to reconstruct paleoclimate and paleoceanographic conditions over geologic time scales. Such... -
Persistent monsoonal forcing of Mediterranean Outflow dynamics during the lat...
The mode and vigor of the global oceanic circulation critically depend on the salinity of (sub)surface water masses advected to the loci of deep-water formation. Within the... -
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... -
Pleistocene chronology of sediments from the Lomonosov Ridge
Despite its importance in the global climate system, age-calibrated marine geologic records reflecting the evolution of glacial cycles through the Pleistocene are largely absent... -
Petrology and geochemistry at DSDP Site 59-448
This chemical and petrologic study of rocks from Site 448 on the Palau-Kyushu Ridge is designed to answer some fundamental questions concerning the volcanic origin of remnant... -
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... -
Carbon/oxygen ratios, clay composition and gas-hydrate saturation of ODP Leg ...
The analyses of downhole log data from Ocean Drilling Program (ODP) boreholes on the Blake Ridge at Sites 994, 995, and 997 indicate that the Schlumberger geochemical logging... -
Analysis of an ancient global warming event, the Paleocene-Eocene thermal max...
Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene... -
P-wave velocities and applied bed thickness and velocity changes for syntheti...
Synthetic seismograms provide a crucial link between lithologic variations within a drill hole and reflectors on seismic profiles crossing the site. In essence, they provide a... -
Nd isotope composition of fossil fish teeth of ODP Hole 119-738B
We report an optimized method for extracting neodymium (Nd) from fossil fish teeth with a single-stage column (125 µl stem volume; LN Resin, Eichrom Industries, Darien Illinois)... -
Geochemistry of serpentenites from DSDP Hole 84-566C
We studied a unique chrysotile–antigorite serpentinite, drilled on Deep Sea Drilling Project Leg 84 (Site 566) in the Guatemala forearc. Our in situ major and trace element data... -
Stable carbon and oxygen isotope record of planktonic foraminifera across the...
The early Cenozoic marine carbon isotopic record is marked by a long-term shift from high d13C values in the late Paleocene to values that are 2 to 3 lower in the early Eocene.... -
Helium concentrations of late Miocene sediments
Throughout the history of the Solar System, Earth has been bombarded by interplanetary dust particles (IDPs), which are asteroid and comet fragments of diameter 1-1,000 µm. The... -
Sedimentology, geochemistry and paleomagnetic of ODP Hole 151-913B
The Eocene and Oligocene epochs (55 to 23 million years ago) comprise a critical phase in Earth history. An array of geological records (Zachos et al., 2001,... -
Total organic carbon, metal concentrations and metal and aluminium ratios in ...
Holocene laminated sediments in Saanich Inlet, British Columbia, are interrupted by frequent, non-laminated, massive layers. These layers may be debris flows released by... -
Total organic carbon, delta13C, biomarker, gas compilations and hopanoids ana...
During the Integrated Ocean Drilling Program (IODP) Expedition 307 for the first time a cold-water coral carbonate mound was drilled down through its base into the underlying... -
Age and clay mineral analysis and trace element concentrations from ODP Sites...
Seismic profiles provide evidence that there has been strong transport by deep-water bottom currents and drift deposition on the northern slope of the South China Sea. Earlier...
