-
Supplementary table 2: Carbonate content of DSDP Site 48-401
This dataset has no description
-
Supplementary table 1: Raw X-ray fluorescence (XRF) core scanning data (Al, C...
This dataset has no description
-
(Table S3) Comparison of the magnitude of the CIEs of PETM, ETM2 and H2 in th...
Asterisk (*) denotes incomplete sequence. -
(Table S2) Linear sedimentation rates preceding and following ETM2 in the Atl...
A significant post-ETM2 reduction is observed everywhere. Sites with () symbols provide estimates while Sites with (*) provide different approximations, based on different age... -
(Appendix A) Abundance of ostracode species from DSDP Hole 48-401
Previous low resolution studies suggest that ostracodes, in contrast with deep sea foraminifera, largely survived the massive environmental changes of the Paleocene–Eocene... -
(Table S1) Stable carbon and oxygen isotope ratios of Nuttallides truempyi of...
An exceptional analogue for the study of the causes and consequences of global warming occurs at the Palaeocene/Eocene Thermal Maximum, 55 million years ago. A rapid rise of... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Neodymium isotope record of late Paleocene to eraly Eocene fish teeth
High-resolution, fish tooth Nd isotopic records for eight Deep Sea Drilling Project and Ocean Drilling Program sites were used to reconstruct the nature of late Paleocene-early... -
Chronostratigraphic summary for Middle Miocene through Pliocene dinoflagellat...
This dataset has no description
-
X-ray fluorescence (XRF) core scanning data (light elements) of core 13 of DS...
This dataset has no description
-
Annotated record of the detailed examination of Mn deposits from DSDP Leg 48 ...
Unlike many cruises of the Deep Sea Drilling Project, Leg 48 was scientifically planned to drill a number of sites to systematically address the problems of passive margin... -
Chemical composition of bottom sediments from DSDP Hole 48-403
This dataset has no description
-
Carbonate associated trace metal and uranium isotope data for the PETM
The Paleocene Eocene Thermal Maximum (PETM) represents a major carbon cycle and climate perturbation that was associated with ocean de-oxygenation, in a qualitatively similar... -
(Table 3) Survey of Atlantic Ocean DSDP sites for hiatuses PH and NH 1 throug...
This dataset has no description
-
Age model and stable isotope record of DSDP holes 48-401 and 86-577
Early Paleogene warm climates may have been linked to different modes and sources of deepwater formation. Warm polar temperatures of the Paleocene and Eocene may have resulted... -
Stable isotopic and carbonate cyclicity in deep sea sediments from different ...
Oxygen and carbon isotopic variability of the dominant (<38 µm) carbonate fraction within bedded, organic-carbon rich Lower Cretaceous sediment intervals from various DSDP... -
Chemical and mineral compositions of sedimentary deposits and magmatic rocks ...
This collective monography by a group of lithologists from the Geological Institute of the USSR Academy of Sciences summarizes materials of the Deep-Sea Drilling Project from... -
Strontium isotope ratios of DSDP samples
The isotopic ratio of strontium-87 to strontium-86 shows no detectable variation in present-day ocean water but changes slowly over millions of years. The strontium contained in... -
Age model and elemental data of DSDP Holes 48-401 and 80-549
A growing body of geologic evidence suggests that emplacement of the North Atlantic Igneous Province (NAIP) played a major role in global warming during the early Paleogene as... -
Chemical composition and dated ages of detrital smectites in sediments at DSD...
Mineralogical, morphological and isotopic (Rb-Sr and K-Ar) determinations were made on some detrital smectites of Palaeocene and Cenomanian ages from DSDP. drillings in the...
