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Meteoric 10Be concentrations and OSL depositional ages of Rio Bermejo floodpl...
To determine the depositional age and the long-term delivery of meteoric 10Be (10Bem) to the Rio Bermejo floodplain (northern Argentina), we collected floodplain sediment... -
(Table 3) Extent of racemization (D/L) in foraminifera from Arctic Ocean sedi...
Ages with two decimals (not *.00) are 14C age; other ages are estimated on the basis of stratigraphic correlations. -
(Table 2) Carbon dioxide record in ice cores from Law Dome and WAIS Divide
Interlaboratory comparison between Oregon State University (OSU) and CMAR (CSIRO Marine and Atmospheric Research,Australia). -
(Table 2, Page 270) Average chemical composition of manganese nodules and cru...
Considerable regional variations in the chemical composition of manganese nodules from a wide range of the Pacific Ocean have been observed. These variations can be more exactly... -
Seawater carbonate chemistry and bioenergetics and disease susceptibility in ...
Pacific herring Clupea pallasii were reared from hatch under 3 CO2 partial pressure (pCO2) treatments (ambient, ~650 μatm; intermediate, ~1500 μatm; high, ~3000 μatm) through... -
Table 1. Compilation and age span of conventional and reservoir-age-corected ...
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Isotopic composition of hydrogen (δD), oxygen (δ¹⁸О) and Deuterium excess in ...
The authors obtained new results on isotope data for recent growing ice wedges on the coast of the Chukotka Peninsula and summarized data from publications of the last 15-20... -
(Table 1) N-isotope record of planktonc foraminifera of sediment core MD02-25...
Constraining variations in marine N2-fixation over glacial-interglacial timescales is crucial for determining the role of the marine nitrogen cycle in modifying ocean... -
(Table 1) Petrology of ODP Hole 125-779A peridotite samples
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(Table 3) Structural specifications of ODP Hole 125-779A peridotite samples
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(Table 2) Petrology of ODP Hole 125-780C peridotite samples
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(Table 4) Structural specifications of ODP Hole 125-780C peridotite samples
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Tab. 4: Palaeomagnetic data for the dykes in the northern and northwestern Sh...
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Tab. 5: Palaeomagnetic results of the Read Mountains Dykes
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Late Cretaceous to Miocene benthic foraminifer δ¹⁸O records and derived botto...
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Stable isotope composition (δ¹⁸О, δ²H and dexc) of massive ice bodies, Easter...
Massive ice (MI) bodies exposed in floodplain and terraces at 7 sites have been studied from 1985 to 2020. In recent research stable oxygen and hydrogen isotope composition of... -
(Table 1) Bolboforma abundance in ODP Hole 162-982B Pliocene sediments
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant: >50 specimens; C = common: 25-50 specimens; R = rare: 2-24 specimens; T = traces: one specimen,... -
(Table 2) Geochemical composition of coals from Dingji Mine
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(Table 3) Elemental abundances in coals from Dingji Mine compared to northern...
References as follows: Dai et al. (2007, doi:10.1007/s11430-007-0001-4); Dai et al. (2008, doi:10.1016/j.coal.2008.01.001); Ren DY, Zhao FH, Dai SF, Zhang JY, Luo KL (2006)... -
Trace elements in Batagay ice wedges, structure ice, Batagaika and Yana River...
Average content of some trace elements in ice wedges, structure ice, Batagaika and Yana River water. Samples were taken rom the Batagay megaslump, 10 km to south east from...
