-
Geochemistry of interstitial water of ODP Hole 186-1151A
This dataset has no description
-
Geochemistry of interstitial water of ODP Hole 186-1150B
This dataset has no description
-
Geochemistry of interstitial water of ODP Hole 186-1150A
This dataset has no description
-
(Supplement S3) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
-
(Supplement S1) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
-
Geochemistry, physical properties, diatom abundance and datums of ODP Site 18...
Detection of climate response to orbital forcing during Cenozoic long-term global cooling is a key to understanding the behavior of Earth's icehouse climate. Sedimentary rhythm,... -
Alkenone composition, UK'37 index, and carbon, sulphur, nitrogen and element ...
Ocean Drilling Program (ODP) Site 1151 (Sacks, Suyehiro, Acton, et al., 2000, doi:10.2973/odp.proc.ir.186.2000) is located in an area where the surface water mass is influenced... -
Stable isotope ratios and geochemical composition of authigenic carbonates fr...
Several carbonaceous layers or fragments were recovered from sediments of Sites 1150 and 1151 on the deep-sea terrace of the Japan Trench during Leg 186. The X-ray diffraction... -
Calcium carbonate, organic carbon, δ¹³C and C/N composition of ODP Sites 186-...
Past changes in sea-surface productivity in the Oyashio Current are evaluated on the basis of abundances of biological constituents in sediments from Leg 186 sites. Organic... -
Description and geochemical composition of tephra layers from ODP Hole 186-11...
The sediments collected at Sites 1150 and 1151 during Leg 186 included many tephra layers and volcaniclastic detritus. In order to identify these tephras, the major oxide... -
Distribution, depositional form and geochemical composition of tephra horizon...
Major element geochemical composition was established for 59 tephra horizons from Ocean Drilling Program Sites 1150 and 1151, located in the Japan forearc. These data,... -
Composite depth scales, ash layer correlations and splice tie points of ODP S...
We present composite depth scales for the multiply cored intervals from Sites 1150 and 1151. These new depth scales place coeval strata recovered in cores from different holes... -
Abundance of stratigraphically important planktic foraminifera and biohorizon...
The planktonic foraminiferal biostratigraphy of Sites 1150 and 1151 drilled in the Japan Trench region during Ocean Drilling Program Leg 186 has been examined. At these drill... -
Dinoflagellate cyst biostratigraphy of ODP Hole 186-1151A sediments
More than 70 dinoflagellate cyst taxa have been encountered in a palynological study of 34 samples from part of the Neogene section of Hole 1151A, Ocean Drilling Program (ODP)... -
Calcareous nannofossil stratigraphy of sediments from ODP Holes 186-1150A and...
To assess the paleoceanographic potential of Leg 186 sediments, we investigated Quaternary calcareous nannofossil flora at Sites 1150 and 1151 in the Japan Trench. Because of... -
Neogene calcareous nannofossil abundance and datums of ODP Site 186-1150 and ...
Calcareous nannofossil assemblages were studied from Ocean Drilling Program Holes 1150A, 1150B, 1151A, 1151C, and 1151D in order to estimate the age of sediments drilled in the... -
Diatom abundance in sediments of ODP Holes 186-1150A and 186-1151C
The diatom flora from two sediment cores recovered from the upper 27 meters below seafloor (mbsf) in the oceanic frontal area off Sanriku, northeast Japan, during Ocean Drilling... -
Miocene to Pleistocene diatom biostratigraphy with a focus on Thalassiosira i...
Late Neogene biostratigraphy of diatoms has been investigated from two sites occupied during Ocean Drilling Program (ODP) Leg 186 off the coast of northeast Japan. A unique... -
Methane concentrations in sediments of ODP sites 186-1150 and 186-1151
Substantial amounts of adsorbed methane were detected in authigenic carbonate concretions recovered from sedimentary layers from depths between 245 and 1,108 m below seafloor... -
Vertical distribution of diatoms in North Pacific sediments
Hydrographic variability in the Mixed Water Region of the Northwest Pacific Ocean at latitudes 35°-40°N, between the Kuroshio Extension and Oyashio Front, causes complex...