8,936 Works

(Table 4) Major and trace element analyses of basalt from DSDP Hole 26-250

Geoffrey Thompson, Wilfred B Bryan, Frederick A Frey, John S Dickey & Hugh L Davies
26-250-26-6,45-47 = Datas from Kempe (1975). The major elements from these sample is recalculated on a volatile-free basis. Trace-elements Datas from these sample are also from Kempe (1975) and Fleet et al. (1976).

(Table 5) Major and trace element analyses of basalt from DSDP Hole 25-249

Geoffrey Thompson, Wilfred B Bryan, Frederick A Frey, John S Dickey & Hugh L Davies
DB1-10 and DB1-11 datas and sample numbers are from Erlank and Reid (1974). The major element from these samples were recalculated on a volatile-free basis.

(Table 2) Major element and trace-element analyses of basalt from DSDP Hole 25-248

Geoffrey Thompson, Wilfred B Bryan, Frederick A Frey, John S Dickey & Hugh L Davies
DB1-8, DB1-9 and DB1-12 datas and sample numbers are from Erlank and Reid (1974). The major elements from these samples were caculated on a volatile-free basis.

Phytoplankton abundance measured on water samples from rivers of the Lena Delta in 2009

Alexandra C Kraberg
During the 2009 cruise in the Lena delta a first comprehensive set of phytoplankton samples was collected from several areas of the Lena Delta. The aim was to establish a first checklist of phytoplankton and microzooplankton species in the Delta for form the basis for future assessments and to aid in the selection of sites to be used as fixed annual monitoring sites in future.

(Table 1) Modal analyses of basalt from DSDP Hole 25-248

Geoffrey Thompson, Wilfred B Bryan, Frederick A Frey, John S Dickey & Hugh L Davies
For rocks in which the groundmass is aphanitic, only the total groundmass is given.

(Table 3) Clinopyroxene and plagioclase analyses from DSDP Hole 26-250

Geoffrey Thompson, Wilfred B Bryan, Frederick A Frey, John S Dickey & Hugh L Davies

Expanded measurements from station Lindenberg (2006-12)

Klaus Behrens
99999: No clouds detected

(Table 2) Paleoelevations of summits of Pacific seamounts 35 million years ago

Lyudmila P Volokitina, Andrey P Sedov & Lev P Zonenshain

(Table 1) Calculated paleoelevations of drillhole points 35 million years ago

Lyudmila P Volokitina, Andrey P Sedov & Lev P Zonenshain

(Table 3) Content of volatile components in the Mid-Atlantic Ridge lithosphere

A S Lapukhov, Vladimir A Simonov & L K Pavlova
H2O in wt %; gases in vol % of their sum.

(Table 6) Distribution of late Eocene calcareous nannofossils in ODP Hole 149-899B

Li Liu
Species abundance: V = very abundant (> 10 specimens per field of view, A = abundant (1 to 10 specimens per field), C = common (1 specimen per 2 to 10 fields), F = few (1 specimen per 11 to 50 fields), R = rare (1 specimen per 51 to 200 fields), - = not present. Sediment depth is given in mbsf.

(Table 7) Distribution of early to middle Eocene calcareous nannofossils in ODP Hole 149-900A

Li Liu
Species abundance: V = very abundant (> 10 specimens per field of view, A = abundant (1 to 10 specimens per field), C = common (1 specimen per 2 to 10 fields), F = few (1 specimen per 11 to 50 fields), R = rare (1 specimen per 51 to 200 fields), - = not present. Sediment depth is given in mbsf.

(Table 5) Distribution of late Eocene calcareous nannofossils in ODP Hole 149-900A

Li Liu
Species abundance: V = very abundant (> 10 specimens per field of view, A = abundant (1 to 10 specimens per field), C = common (1 specimen per 2 to 10 fields), F = few (1 specimen per 11 to 50 fields), R = rare (1 specimen per 51 to 200 fields), - = not present. Sediment depth is given in mbsf.

(Table 3) Distribution of middle Eocene calcareous nannofossils in ODP Hole 149-897C

Li Liu
Species abundance: V = very abundant (> 10 specimens per field of view, A = abundant (1 to 10 specimens per field), C = common (1 specimen per 2 to 10 fields), F = few (1 specimen per 11 to 50 fields), R = rare (1 specimen per 51 to 200 fields), - = not present. Sediment depth is given in mbsf.

(Table 2) Position of the upper and lower boundaries of the seasonal thermocline, and C. fusus population

A S Mikaelyan & T A Zav'yalova
H2O in wt %; gases in vol % of their sum.

(Table 4) Distribution of middle Eocene calcareous nannofossils in ODP Hole 149-897D

Li Liu
Species abundance: V = very abundant (> 10 specimens per field of view, A = abundant (1 to 10 specimens per field), C = common (1 specimen per 2 to 10 fields), F = few (1 specimen per 11 to 50 fields), R = rare (1 specimen per 51 to 200 fields), - = not present. Sediment depth is given in mbsf.

(Table 4) Rare earth element composition of ferromanganese nodules and crusts

Eric Heinen De Carlo & Neville F Exon
Concentrations expressed in µg/g solid phase on a 110°C dried basis.

Registration Year

  • 2011
    8,936

Resource Types

  • Dataset
    8,018
  • Collection
    918