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(Table 1) Initial survey of palynomorph distribution in samples of DSDP Hole ...
This dataset has no description
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(Table 2) Initial survey of palynomorph distribution in samples of DSDP Hole ...
This dataset has no description
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Annotated record of the detailed examination of Mn deposits from DSDP Leg 96 ...
The Mississippi Fan is a broad, arcuate accumulation of Pleistocene deep-water sediments deposited in the eastern Gulf of Mexico. Major objectives for drilling the Mississippi... -
Alkenone-derived Holocene Sea Surface Temperature database
see dating methoda: Correlation with GISP2 oxygen isotope record (Grootes and Stuiver, 1997).b: The age model of the core AD91-17 is based on AMS 14C, planktonic isotopic record... -
Summary of sea surface temperature trends reconstructed from alkenones for th...
Trend >0 means a warming over the time period, trend <0 means a cooling over the time period. -
Expanded GHOST database
In this study we review a global set of alkenone- and foraminiferal Mg/Ca-derived sea surface temperatures (SST) records from the Holocene and compare them with a suite of... -
(Table 1) Major inorganic oxides and trace elements in DSDP Leg 96 holes
This dataset has no description
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(Table 1) Element concentrations in pore-water samples, DSDP Leg 96
This dataset has no description
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(Table 1) Interstitial water chemistry of DSDP Leg 96 holes
This dataset has no description
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Alkenones and reconstructed sea surface temperature from sediment core 96-619...
The sedimentary record of a ratio (UK37) of long chain (C37) unsaturated alkenones is a useful indicator of glacial-interglacial climatic change in the Late Quaternary northern... -
Mineralogy and incipient diagenesis of Pigmy Basin sediments, DSDP Hole 96-619
Pigmy Basin sediments cored in Hole 619 of Deep Sea Drilling Project Leg 96 are silty clays composed, on the average, of < 1% sand, 37% silt, 48% clay, and 14% carbonate... -
Gas hydrates of the Gulf of Mexico
Gas hydrates were recovered from eight sites on the Louisiana slope of the Gulf of Mexico. The gas hydrate discoveries ranged in water depths from 530 to 2400 m occurring as... -
Organic biomarker compound concentrations in sediments from DSDP Hole 96-619
A study of organic biomarker compounds which could serve as tracers of terrigenous and marine sedimentary organic matter sources was performed on samples from a 208.7 m... -
Physical properties and bulk organic geochemical results for sediments from D...
The concentration and carbon isotopic composition (d13C) of sedimentary organic carbon (C_org), N/C ratios, and terrigenous and marine d13C_org endmembers form a basis from... -
(Table 6) Distribution of calcareous nannofossils in DSDP Hole96-624
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 5) Distribution of calcareous nannofossils in DSDP Hole 96-623
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 2) Distribution of calcareous nannofossils in DSDP Hole 96-622
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 1) Distribution of calcareous nannofossils in DSDP Hole 96-621
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 4) Distribution of calcareous nannofossils in DSDP Hole 96-620
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 11) Distribution of calcareous nannofossils in DSDP Hole 96-619
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1...