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Late Eocene to early Oligocene oxygen and carbon isotope records and biogenic...
The late Eocene through early Oligocene (40-33 Ma) represents a transition from a warm-house to icehouse climate mode, with the expansion of Antarctic glaciation shortly after... -
Middle Eocene astronomically-tuned benthic stable isotopes, bulk stable isoto...
To come to a coherent middle Eocene timescale for the Atlantic, we re-evaluate the astrochronology of chrons C20n/C20r at International Ocean Discovery Program (IODP) Expedition... -
Mean dust grain size variations of sediment core PS75/056-1 from the Pacific ...
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Organic geochemical investigation of sediments in the Japan Sea: Tracking pal...
The mid- to late Miocene marks one of the last warm periods of the Neogene, before the descent in to the ice house climate of the late Pliocene and Pleistocene. The mid- to late... -
Sea surface temperature estimates for sediment cores in the Japan Sea
Organic sea surface temperature proxies, UK'37 and TEX86, were used to reconstruct sea surface temperatures in the Japan Sea for the last 17 million years. Data was generated... -
Fish tooth and sediment-derived neodymium isotopes and rare earth element dat...
We assess early-to-middle Eocene seawater neodymium (Nd) isotope records from seven Southern Ocean deep-sea drill sites to evaluate the role of Southern Ocean circulation in... -
Morphometric data for Globigerinoides sacculifer and Globorotalia tumida (siz...
Sediment samples from both Site 165-999/165-1000 (Atlantic) and Site 202-1241 (Pacific) were chosen at 1Ma intervals over the period 0.3-9.3Ma. Samples were washed and sieved... -
Friction analysis of Costa Rica ocean sediments from ODP Hole 170-1039B, 170-...
Seismicity patterns offshore Costa Rica (Central America) at the Middle America Trench have led to speculation that large (moment magnitude, Mw ~7.0) earthquakes are associated... -
Measurements of velocity-dependent and slip-dependent frictional strength in ...
Slowslip forms part of the spectrum of fault behaviour between stable creep and destructive earthquakes. Slow slip occurs near the boundaries of large earthquake rupture zones... -
Sea surface temperatures during Marine Isotope Stage (MIS) 11
The Marine Isotope Stage (MIS) 11 (424-374 ka) was characterized by a protracted deglaciation and an unusually long climatic optimum. It remains unclear to what degree the... -
Dinoflagellate cyst counts and age model from sediment samples of ODP Hole 17...
Sediment samples from ODP Site 1085 were investigated in order to obtain more information on the initiation and development of the Benguela upwelling system during the middle... -
Late Cenozoic eolian dust accumulation in the eastern equatorial Pacific Ocean
Sediments recovered during Ocean Drilling Program (ODP) Leg 138 in the eastern equatorial Pacific Ocean were analyzed for variations in eolian accumulation rate and mean... -
Permeability measurements on sheared and unsheared samples from different IOD...
At subduction zones, the permeability of major fault zones influences pore pressure generation, controls fluid flow pathways and rates, and affects fault slip behavior and... -
Consolidation properties and permeability values of sediments from three ODP ...
Vertical permeability and sediment consolidation measurements were taken on seven whole-round drill cores from Sites 1253 (three samples), 1254 (one sample), and 1255 (three... -
Carbonate preservation of sediment cores from the Great Bahama Bank
The oceanic carbon cycle mainly comprises the production and dissolution/ preservation of carbonate particles in the water column or within the sediment. Carbon dioxide is one... -
Geochemistry of secondary carbonates in ODP Leg 115 basalts
This report presents the results of a study of the stable isotopic and chemical composition of secondary carbonate minerals precipitated within basalts at Ocean Drilling Program... -
Chemical and Sr isotopic compositions and timing of carbonate mineral precipi...
The strontium isotope ratios of authigenic carbonates from Indian Ocean sea-floor basalts have been used to determine the timing of carbonate mineral precipitation and fluid... -
Mid-Pliocene deep-sea bottom water temperatures based on ostracode Mg/Ca ratios
We studied magnesium:calcium (Mg/Ca) ratios in shells of the deep-sea ostracode genus Krithe from a short interval in the middle Pliocene between 3.29 and 2.97 Ma using deep-sea... -
(Table 1) Stontium isotope ratios for ODP Leg 133 sediments
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(Table 1) Geotechnical stratigraphic units of ODP Hole 120-751A
This dataset has no description