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(Table 4) Distribution and abundance of Cretaceous nannofossils in DSDP Hole ...
DEPTH, sediment [m] is given in mbsf. Species abundance: A = abundant (>10 specimens per field ov view at 780 X), C = common (1 specimen per field), F = few (1 specimen per... -
(Table 2) Nannoplankton occurrences in DSDP Hole 89-586B
Sediment depth is given in mbsf. Species abundance: A = abundant (>50 specimens), C = common (25-49 specimens), and R = rare (<25 specimens) - = absent, obtained by... -
(Table 3) Benthic foraminifera in early-middle Miocene sediments of DSDP Site...
Abundances: X = present, A = very abundant, - = absent. -
(Table 2) Benthic foraminifera in Pliocene sediments of DSDP Hole 89-586B
Abundances: X = present, A = very abundant, - = absent. -
(Table 1) Benthic foraminifera in late Miocene sediments of DSDP Hole 89-586B
Abundances: X = present, A = very abundant, - = absent. -
(Table 2) Distribution of Cretaceous redeposited benthic foraminifers at DSDP...
Abundances based on total fauna recovered from 20-cm**3 samples greater than 42 µm. -
(Table 1) Distribution of Cretaceous redeposited benthic foraminifers at DSDP...
Abundances based on total fauna recovered from 20-cm**3 samples greater than 42 µm. -
(Table 2) Distribution and abundance of late Cretaceous to early Paleocene na...
DEPTH, sediment [m] is given in mbsf. Species abundance: A = abundant (>10 specimens per field ov view at 780 X), C = common (1 specimen per field), F = few (1 specimen per... -
(Table 1) Distribution and abundance of late Cretaceous to middle Eocene nann...
DEPTH, sediment [m] is given in mbsf. Species abundance: A = abundant (>10 specimens per field ov view at 780 X), C = common (1 specimen per field), F = few (1 specimen per... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
(Figure 3) Distribution of latest Aptian and Cenomanian-Turonian planktonic f...
X = present, ? quetionable occurrence, r = reworked, - = absent. -
(Table 8E) Occurrences of planktonic foraminifers in selected samples of DSDP...
X = present, - = absent, cf. = confer, R = reworked. -
(Table 8D) Occurrences of planktonic foraminifers in selected samples of DSDP...
X = present, - = absent, cf. = confer, R = reworked. -
(Table 8C) Occurrences of planktonic foraminifers in selected samples of DSDP...
X = present, - = absent, cf. = confer. -
(Table 8B) Occurrences of planktonic foraminifers in selected samples of DSDP...
X = present, - = absent, cf. = confer, R = reworked. -
(Table 8A) Occurrences of planktonic foraminifers in selected samples of DSDP...
X = present, - = absent, cf. = confer. -
Data compilation of bio-SiO2 MAR from 21 sites
The table includes complicated bio-SiO2 MAR from 21 sites in the global ocean during the late Miocene. We also use Geologic Time Scale 2020 timescale (Gradstein et al., 2020;... -
Synthesis of early Pliocene and mid-Pliocene carbon anomaly
This dataset has no description
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(Table 5) Distribution and abundance of early Cretaceous nannofossils in DSDP...
DEPTH, sediment [m] is given in mbsf. Species abundance: A = abundant (>10 specimens per field ov view at 780 X), C = common (1 specimen per field), F = few (1 specimen per...
