-
(Table 14) Ranges of benthic foraminifers through the Neogene 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 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 8) 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 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... -
(Appendix B2) Diversity and acculmulation rates of radiolarian faunas across ...
This dataset has no description
-
(Appendix B1) Diversity and acculmulation rates of radiolarian faunas across ...
This dataset has no description
-
(Table 2) Abundance of ostracods in surface sediment samples from the Admiral...
Sampling depth 0-15 cm. Each separate valve was counted as one specimen. Fragmented valves were 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
-
Megabenthic composition and associated environmental variables of the Charlie...
These data include the species matrix and all associated environmental variables (Slope, depth, temperature, salinity, substrate type) of all observed megabenthic species from... -
Hydromorphological conditions of small streams in North Italy and West Austria
Considering the entire fluvial network of Tyrol and South Tyrol, 81 sampling sites were selected according to the following requirements: (1) degree of hydrological disturbance... -
Vascular plant species richness along a climate and land-use gradient in Mong...
The data set features the species richness of vascular plants along a 600km long gradient Mongolian rangeland vegetation. The data was collected to study the role of climatic... -
Recruit abundance on a long-term experiment (1999-2017) in the LTER observato...
These data represent the results of a long-term colonization experiment at the Long-Term Ecological Research observatory HAUSGARTEN. Recruitment panels were constructed from...