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Mineral composition of clay fraction from Hole 79-544
This dataset has no description
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Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Sedimentology of sites 14-141, 41-366, 47-397 and 79-544B
Along the N-S-transect of DSDP-Sites 5446, 397, 141, and 366, oxygen and carbon isotopes, flux rates of calcium carbonate, terrigenous matter, and biogenic opal, clay minerals... -
Jurassic microfossils of DSDP Hole 79-547B
The first marine incursion of the incipient North Atlantic Ocean is recorded in the uppermost Triassic to Lower Jurassic sequence of DSDP Site 547 off central Morocco. A... -
Major and trace elements and minerals at DSDP Hole 79-544A
Fifty m of basement rocks underlying 185 m of Neogene and Mesozoic sediments were drilled seaward of the Mazagan Slope about 100 km west of Casablanca during Leg 79. These rocks... -
Geochemistry and isotopes at DSDP Hole 79-546
At Site 546, below the Mazagan Escarpment at a water depth of 4 km, 36 m of salt rock was cored from the top of one of a field of salt domes. The core was studied by thin... -
Early Cretaceous large, few-chambered Globigerinelloides from the Tethys
New findings of well-preserved Early Cretaceous planktonic foraminiferal assemblages from the Cismon core (NE Italy), Calabianca (NW Sicily), Lesches en Diois (SE France) and... -
Early Cretaceous large, many-chambered Globigerinelloides from the Tethys
This paper deals with the taxonomic revision of the Early Cretaceous large, many-chambered planispiral planktonic foraminifera, historically assigned to the genus... -
Early Cretaceous planktonic foraminifera from the Tethys
Early Cretaceous planktonic foraminiferal assemblages include rare planispiral and pseudoplanispiral morphotypes with elongate chambers that BouDagher-Fadel et al. assigned to... -
Depth, age, strontium isotopic ratios and trace elemental ratios of samples f...
Large variations exist between published mid-Cretaceous (late Barremian to early Turonian stages) seawater Sr-isotope stratigraphies; this has resulted in disparate... -
Stable chlorine isotopes in pore waters from DSDP Hole 79-546 and ODP Hole 13...
Stable Cl isotope ratios, measured in marine pore waters associated with the Barbados and Nankai subduction zones, extend significantly (to ~-8 per mil) the range of d37Cl... -
Integrated stratigraphy of the Messinian across the North Atlantic Ocean
The Messinian was a time of major climatic and paleoceanographic change during the late Cenozoic. It is well known around the Mediterranean region because of the giant... -
Foraminifera and microfossil occurence in Late Jurassic sediments of the Nort...
Biostratigraphical, taxonomical, and palaeocological results were obtained from Oxfordian to Tithonian foraminifers of the Northern and Southern Atlantic Ocean boreholes of the... -
Stable isotope ratios of benthic foraminifera from DSDP Hole 79-544B (Table 1)
At DSDP Hole 544B, oxygen-isotope stratigraphy, carbonate proportion, clay mineralogy, and (terrigenous) grain sizes show short-term (Milankovitch-type) sediment cycles from 5.1... -
Calcareous nannofossils absolute abundance and accumulation rates from DSDP S...
This dataset has no description
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(Figure 5) Distribution and relative abundances of microbiota recovered from ...
Species abundance: F = few (1-3 specimens), C = common (4-9 specimens), A = abundant (>10 specimens), X = present, - = absent. -
(Figure 4) Distribution of dinoflagellate cysts in the Albian/Cenomanian of D...
Species abundance: D = dominant (>100 specimens), A = abundant (51-100), C = common (21-50), F = few (4-20), R = rare (1-3), - = absent. -
(Figure 3) Distribution of dinoflagellate cysts in the late Albian of DSDP Ho...
Species abundance: D = dominant (>100 specimens), A = abundant (51-100), C = common (21-50), F = few (4-20), R = rare (1-3), - = absent. -
(Figure 1) Distribution of dinoflagellate cysts in the mid-Cretaceous of DSDP...
Species abundance: D = dominant (>100 specimens), A = abundant (51-100), C = common (21-50), F = few (4-20), R = rare (1-3), - = absent. -
(Table 3) Distribution of Cretaceous nannofossils at DSDP Hole 79-547A
Species abundance: D = very abundant (10 or more specimens per field of view)), A = abundant (6-9 specimens per field), V = very common (3-5 specimens per field)), C = common (1...
