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(Table 13) Ranges of benthic foraminifers through the early to middle Miocene...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 12) Ranges of benthic foraminifers through the Miocene in ODP Hole 115...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 11) Ranges of benthic foraminifers through the Oligocene in ODP Hole 1...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 10) Ranges of benthic foraminifers through the Oligocene in DSDP Hole ...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 9) Ranges of benthic foraminifers through the Oligocene in ODP Hole 11...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 6) Ranges of benthic foraminifers through the Oligocene in DSDP Hole 2...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 5) Ranges of benthic foraminifers from the late Oligocene to the early...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 4) Ranges of benthic foraminifers from the early Oligocene to the earl...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 3) Ranges of benthic foraminifers from the late Eocene through the Oli...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
Late Albian Col de Palluel (SE France, Niveau Breistroffer): range chart in p...
values with <1 = rare occurence, not counted -
(Table 2) Relative abundance and occurence for selected siliceous microfossil...
r = Reworked: rare occurence of a taxon noted and interpreted as reworked; fr = Fragment: rare fragment(s) of the taxon present; X = Present: complete specimens rare (=< 1... -
Percentage of nannoplankton of sediment core Kronsmoor, Late Cretaceous
This dataset has no description
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Living coccolithophore abundance from the Ebro Delta coastal area during MERS...
The present dataset contains coccolithophores abundances (coccospheres/L). The samples were collected between Barcelona and the Ebro Delta (Western Mediterranean), during the... -
Bioengineering experiment on Schiermonnikoog 2015: experimental effects on di...
In 2015 the Marine Ecology lab. (Eriksson Lab. at the Groningen Institute for Evolutionary Life Sciences [GELIFES], University of Groningen, The Netherlands); tested the effect... -
Manipulation experiment on phytoplankton diversity, species composition and b...
Ecological research in recent decades revealed that species loss has a predominantly negative effect on ecosystem functioning and stability. Most of these studies were based on... -
(Table 3) Collembola species density and diversity in control and OTC plots n...
Ecosystems at high northern latitudes are subject to strong climate change. Soil processes, such as carbon and nutrient cycles, which determine the functioning of these... -
(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... -
(Appendix A) Nannofossil stratigraphic range chart for the late Maastrichtian...
The response of calcareous nannofossils to the end-Cretaceous warming is investigated in the Tropical Pacific DSDP Site 577A (Shatsky Rise) through the record of species... -
(Appendix A) Radiolarian abundance in ODP Hole 202-1241A
A quantitative radiolarian study at Ocean Drilling Program Site 1241 in the eastern tropical Pacific enables us to reconstruct paleoceanographic changes that occurred since the... -
Range chart of calcareous nannofossils from ODP Hole 188-1165B (Table 1)
Bio- and magnetostratigraphic age data and nannofossil assemblage analysis from ODP Site 1165 evidence an anomalous warming event of the surface waters in and around Prydz Bay...
