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(Figure 1) Dinoflagellate cyst stratigraphy of DSDP Hole 80-548A
Cyst assemblages from Sites 548, 549, and 550 were examined and gave evidence of early Eocene to late Miocene age. These assemblages were compared with other North Atlantic... -
(Table 1) Occurrences of volcanic ash at DSDP Leg 78A Holes
Air-fall volcanic ash recovered at Deep Sea Drilling Project Sites 541, 542, and 543 on and east of the toe of the Barbados Ridge delineate middle and late Miocene, early... -
(Table 2) Distribution of phytoliths in selected samples from DSDP Site 90-591
Phytoliths are described from deep sea sediments at Site 591 in the southwestern Pacific. Their regional distribution is related to the arid and semiarid regions of Australia,... -
(Table 2) Sub-bottom depths, biostratigraphic zones, and ages for major refle...
The analysis of high-resolution watergun seismic profiles collected in support of DSDP Leg 85 drilling reveals several major, regionally traceable reflectors that can be... -
(Table 2) Biostratigraphic and magnetostratigraphic age model for ODP Sites 1...
Carbonate content and mass accumulation rate (MAR) were determined for Holes 998A, 999A, and 1000A recovered during the Ocean Drilling Program (ODP) Leg 165 in the Yucatan Basin... -
(Table 2) Major and trace elements in the ash layer at DSDP Sample 95-613-34-...
A 2-5-cm-thick, middle to lower middle Eocene, vitreous ash layer of rhyolitic composition can be correlated between Sites 605 and 613 on the uppermost continental rise off New... -
(Table 1) Distribution of Lower Cretaceous calcareous nannofossils at DSDP Ho...
Upper Berriasian to lower Aptian calcareous nannofossil assemblages have been studied from a siliciclastic deep-sea fan complex and a subjacent limestone sequence drilled... -
(Table T1) Biostratigraphy and distribution of Quaternary and Miocene calcare...
During Ocean Drilling Program (ODP) Leg 188, piston and rotary cores were recovered at three southern Indian Ocean sites on the continental margin in Prydz Bay, Antarctica, in... -
Distribution of calcareous nannofossils from IODP Hole 313-M0029A
Sediment depth is given in mbsf. Abundance: V = very abundant, A = abundant, C = common, Fr = frequent, F = few, R = rare; B = barren; ? = questionable; * = reworked.... -
Distribution of calcareous nannofossils from IODP Hole 313-M0028A
Sediment depth is given in mbsf. Abundance: A = abundant, C = common, Fr = frequent, F = few, R = rare, B = barren, ? = questionable, * = reworked. Preservation: G = good, M =... -
Distribution of calcareous nannofossils from IODP Hole 313-M0027A
Sediment depth is given in mbsf. Abundance: V = very abundant, A = abundant, C = common, Fr = frequent, F = few, R = rare, B = barren, ? = questionable, * = reworked.... -
(Appendix) Late Cretaceous calcareous nannofossils of DSDP Holes 80-549 and 8...
he early late Cretaceous (Cenomanian–early Turonian) is thought to have been one of the warmest periods of the Phanerozoic. This period was characterised by tropical sea surface... -
(Table T1) Distribution of selected calcareous nannofossils at the Paleocene/...
Ocean Drilling Program Leg 208 Hole 1266C (28°32.55'S, 2°20.61'E) is located along the northwestern flank of Walvis Ridge (South Atlantic Ocean). The location of Site 1266, at... -
(Table 1) Biostratigraphic zonation and core depth of microtektite occurrence...
Microtektites have been recovered from three horizons in eight middle Eocene to middle Oligocene marine sediment sequences. Five of these occurrences are coeval and of latest... -
(Table 1) Trace element concentrations and Sr isotope ratios of carbonates
Measurements of marine carbonate samples indicate that during the past 2.5 million years the 87Sr/86Sr ratio of seawater has increased by 14 * 10**-5. The high average rate of... -
(Table 2) Occurrence of the most abundant nannofossil taxa in middle Cretaceo...
Middle Cretaceous calcareous nannofossils were quantitatively studied at Sites 800, 801, and 802 of Leg 129. Samples were selected after careful inspection of the total... -
Distribution of calcareous nannofossils in the lower sequence of the CIROS-1 ...
Semiquantitative data of calcareous nannofossil species abundance were collected for 31 samples from 380.00 to 696.61 m below sea floor (mbsf) in the CIROS-1 core from the... -
Abundance of calcareous nannofossils across the K/T boundary at ODP Hole 113-...
A biostratigraphically continuous, but intensely bioturbated, Cretaceous/Tertiary boundary sequence was cored during Ocean Drilling Program (ODP) Leg 113 on Maud Rise (65°S) in... -
Distribution of sponge spicule types, Goniothecium odontella and Diploneis cf...
Clusters of sponge spicules found in Quaternary deep-water sediments at Sites 685 and 688 off Peru represent single individuals of small sponges or fragments of larger sponges.... -
Distribution of late Neogene age calcareous nannofossils in ODP Hole 111-677A...
The calcareous nannofossil assemblages recovered from Site 677A range in age from latest Miocene (NN11) to latest Pleistocene. The consistently high sediment-accumulation rate...
