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(Supplementary Table 1) Iceberg-rafted debris (IBRD) mass accumulation rates ...
The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a transition from a global climate state that was 2-3 °C warmer than present with limited ice... -
(Table 2) Carbonate chemistry and isotopes from northern Cascadia margin samples
Most authigenic carbonates previously recovered from the Cascadia slope have 87Sr/86Sr signatures that reflect shallow precipitation in equilibrium with coeval seawater. There... -
(Table 1) Sediment composition, description and texture at DSDP Hole 93-603B
A 300-m-thick, upper Valanginian to Barremian turbidite sequence, consisting of sandstone and organic-matter-rich claystone turbidites intercalated in pelagic marl and... -
(Table S1) Stable carbon isotope composition of dissolved inorganic carbon an...
We studied microbially mediated diagenetic processes driven by carbon mineralization in subseafloor sediment of the northeastern Bering Sea Slope to a depth of 745 meters below... -
(Table 1) Depth and ages of the chronolostratigraphical boundaries from IODP ...
Cores raised during IODP Expedition 303 off southern Greenland (Eirik Ridge site 1305) and off the Labrador Coast (Orphan Knoll site 1302/1303) were analyzed to establish an... -
Lithic grain and mineral composition of sand and sandstones from the North Pa...
Sand and sandstone compositions from different types of basins reflect provenance terranes governed by plate tectonics. One hundred and one thin sections of Upper Miocene to... -
Distribution of foraminiferal fauna from ODP Hole 122-762C (Table 1)
Planktonic foraminiferal diversity, equitability and biostratigraphic analysis of samples from Ocean Drilling Program (ODP) Leg 122, Hole 762C show that in general, cool water... -
(Table A1) CaCO3 contents and Sr/Ca ratios in ODP Leg 130, 138 and 154
Strontium/calcium (Sr/Ca) ratios in bulk and foraminiferal calcite have been used to constrain the history of Sr/Ca in the oceans and to evaluate calcite diagenetic alteration.... -
Age determination of sediment core NP90-52 (Table 1)
Data on glacial erosion have been compiled and synthesised using a wide range of sediment budget and sediment yield studies from the Svalbard-Barents Sea region. The data... -
(Table 1) Age model of ODP Site 184-1144
Variations in nitrogen isotopic composition (d15N) and total chlorin accumulation rate (AR) are employed asproxies to reconstruct oceanic nitrate inventory, the balance between... -
(Table 1) Summary statistics of taxa in samples of ODP Hole 181-1123B
Planktonic foraminifera are used to identify late Pliocene-Quaternary near surface water masses on the northeastern flank of Chatham Rise by comparison with faunas in core-tops... -
(Table 1) Viscosity coefficients at various temperatures of samples from ODP ...
Ocean Drilling Program (ODP) Hole 735B was drilled to a depth of 1.5 km in a tectonic window of gabbroic lower oceanic crust created at the Southwest Indian Ridge. The gabbros... -
(Table DR1) Biofacies, percentages of important benthic foraminifera and isot...
The Indian monsoon system, as recorded by ocean-floor biota (benthic foraminifera) at Ocean Drilling Program Site 758 in the eastern equatorial Indian Ocean, has varied... -
Rock eval analysis of organic matter in sediment core 159-959D
The Cretaceous Equatorial Atlantic Gateway between the Central and South Atlantic basins is of interest not only for paleoceanographic and paleoclimatic studies, but also... -
Utility of thallium and geochemical analysis of Mariana arc sediments from OD...
We provide the first exploration of thallium (Tl) abundances and stable isotope compositions as potential tracers during arc lava genesis. We present a case study of lavas from... -
Geochemical analysis on lavas from Nevado de Toluca, Central Mexican Volcanic...
This study presents evidence that Quaternary frontal arc calc-alkaline lavas from Central Mexican Volcanic Belt (CMVB) contain contributions from partial melts of the subducting... -
Zircons, isotope ratios and element analyses from tonalite and oxide gabbro o...
A limiting factor in the accuracy and precision of U/Pb zircon dates is accurate correction for initial disequilibrium in the 238U and 235U decay chains. The longest-lived-and... -
Geochemistry, lithology and maceral analysis at DSDP Hole 71-511
The quantity, type, and maturity of the organic matter in Recent through Upper Jurassic sediments from the Falkland Plateau, DSDP Site 511, have been determined. Sediments were... -
Trace and rare elements and factors at DSDP Hole 71-511
The distribution of paragenetic assemblages of trace and rare elements, as revealed by factor analysis (R-mode, Q-mode), the ratios of elements to Zr and the interpretation of... -
Carbonate compensation depth (CCD) reconstruction of the equatorial Pacific
Atmospheric carbon dioxide concentrations and climate are regulated on geological timescales by the balance between carbon input from volcanic and metamorphic outgassing and its...
