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Pollen analysis of ODP Hole 108-658B
This dataset has no description
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Pollen analysis of ODP Hole 108-658A, Part II
This dataset has no description
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Pollen analysis of ODP Hole 108-658A, Part I
This dataset has no description
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Pollen analysis of ODP Hole 108-658A
This dataset has no description
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Pollen analysis of ODP Hole 202-1239A
Vegetation and climate change in western equatorial South America were studied using palynological analysis. We studied 88 marine sediment samples from ODP Site 1239 dated... -
Dinoflagellate cyst counts of ODP Site 1081, Benguela Upwelling, Miocene-Plio...
Using the Late Miocene to Pliocene organic-walled dinoflagellate cyst record of ODP Site 1081 we reconstruct and discuss the early upwelling history over the Walvis Ridge with a... -
Pollen and spores of ODP Hole 175-1081A, Miocene-Pliocene, Walvis Ridge
Aridification is an important component of Late Neogene climate change in south-western Africa probably caused by modifications in the atmospheric circulation in relation to the... -
(Table S3) Benthic foraminiferal Mg/Ca, Li/Ca and stable isotope ratios of OD...
The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate saturation state have recently been assessed. Here we present a new approach... -
(Table 1) I, Br, B, d11B and Mn concentrations in ODP Site 131-808
This study of the interstitial water concentration-depth distributions of iodide, bromide, boron, d11B, and dissolved organic carbon, as represented by absorbance at 325 nm... -
(Table 1) Age determination of ODP Leg 166 holes
Thick, late Quaternary sediment sections were recovered at several sites on the leeward slope of Great Bahama Bank during Leg 166 of the Ocean Drilling Program. These sections... -
Pollen abundance in ODP Site 123-765 (Table 1)
Middle Miocene to Holocene pollen assemblages reveal a history of environmental change in northern Australia. Grass pollen appeared, but was rare, in the late Miocene and was... -
Pollen analysis of ODP Hole 117-720A (Appendix B)
Pollen analytical studies of the ODP Site 720 cores revealed the wide development of the coniferous forest, which mainly composed by Pinus, Picea, Abies and Cedrus deodara,... -
Age, pollen and spores of ODP Site 175-1082
The present-day condition of bipolar glaciation characterized by rapid and large climate fluctuations began at the end of the Pliocene with the intensification of the Northern... -
Pollen analysis of ODP Hole 159-958A
Palynological investigation (pollen, spores, and dinoflagellate cysts) of 39 samples from the upper 50 m of Ocean Drilling Program (ODP) Site 958 provides some complementary... -
Carbonate minerals, uranium and thorium concentration and U-Th ages of sedime...
We have performed U-Th isotope analyses on pure aragonite samples from the upper sections of Leg 166 cores to assign each aragonite-rich sediment package to the correct... -
n-Alkane, fatty acid and hopanoic acid concentrations of ODP Site 190-1178 sa...
Ocean Drilling Program (ODP) Leg 190 was programmed to investigate deformational, diagenetic, and hydrologic processes and their interactions in the Nankai Trough accretionary... -
Oxygen isotopic composition of interstitial waters from ODP Leg 207 sites
We determined oxygen isotopic compositions of interstitial water (IW) recovered during Ocean Drilling Program Leg 207. Five sites were cored (3200- to 1900-m water depth) on... -
Fluorescence of dissolved organic matter un marine sediments
The fluorescence of porewaters from marine sediment cores from six different areas was measured. In most cases, fluorescence was affected primarily by the diagenesis of organic... -
Composition of hardgrounds and of pore-water parameters in ODP Holes 166-1008...
Mineralogic, petrographic, and geochemical analyses of sediments recovered from two Leg 166 Ocean Drilling Program cores on the western slope of Great Bahama Bank (308 m and 437... -
Uranium concentrations and isotope ratios Bahamas seawater and ODP holes pore...
The geometry, timing, and rate of fluid-flow through carbonate margins and platforms is not well constrained. In this study, we use U concentrations and isotope ratios measured...