-
Paleoceanographic changes based on radiolarians of ODP Site 115-710 from the ...
This dataset has no description
-
Freshwater zooplankton abundance in different water bodies from a polygonal t...
Patterned ground of the polygonal tundra yields sensitive indicators of environmental and climate change. Polygon ponds, mires and cryosoils are typical components of Arctic... -
Nannofossil assemblage of IODP Site 356-U1463
This dataset has no description
-
Abundance and diversity of coccolithophores from the Java upwelling system (c...
This dataset has no description
-
(Table 3) Abundances, dominance and diversity of benthic meiofauna sampled in...
Unit originally given in #/10 cm² -
(Table S2) Palynomorph counts of DSDP Hole 94-610A
DEPTH, sediment/rock [m] is given in mbsf. Samples were counted until more than 200, and often more than 300, dinoflagellate cysts had been enumerated. A <1 in the data set... -
(Appendix) Radiolarian abundances in ODP Hole 171-1052A
This dataset has no description
-
Late Albian Col de Palluel (SE France, Niveau Breistroffer): range chart in p...
values with <1 = rare occurence, not counted -
Benthic foraminifera diversity of the abyssal Northwest Atlantic
Foraminiferal assemblage data was collected from thirty-two samples of seven cores of 0 cm down to 30 cm from the abyssal Northwest Atlantic. The investigated material was... -
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... -
(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 2) Megafauna density 2002, 2004 and 2007 in the deep-sea observatory A...
Although megafaunal organisms play an important role in deep benthic ecosystems and contribute significantly to benthic biomass in the Arctic little is known about their... -
(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... -
(Appendix A) Campanian-Maastrichtian calcareous nannofossils in DSDP Hole 44-...
The latest Cretaceous (Campanian–Maastrichtian) is characterized by several global cooling and intermittent warming events. These climatic changes influenced the... -
Palynology of sediment cores from site GS15-198-38
This dataset has no description
-
(Table 2) Abundances, dominance and diversity of benthic macrofauna sampled i...
Unit originally given in #/100 cm² -
(Table S1) Palynomorph counts of IODP Hole 303-U1308C
DEPTH, sediment/rock [m] is given in mbsf. Samples were counted until more than 200, and often more than 300, dinoflagellate cysts had been enumerated. A <1 in the data set... -
Quantitative analysis of the Eocene record from IODP Hole 318-U1356A
Sediment depth is given in mbsf. Only samples with 100 and more individuals are presented. -
(Fig. 4) Relative proportions of the most abundant chironomid taxa in the Lak...
This dataset has no description
-
Tab. 5: Artenzusammensetzung, mittlere Individuendichte, Diversität und Evene...
This dataset has no description
