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(Table 3) Mollusc biostratigraphy of facies overlying the 'Braunkohlensande' ...
Depth, sediment represents the mean of the depth ranges. X = present, - = absent. -
(Table 2) Mollusc biostratigraphy of facies underlying the 'Braunkohlensande'...
Depth, sediment represents the mean of the depth ranges. X = present, - = absent. -
(Tab 3) Signal to noise ratio (SNR) by genus for microarray probes in an allu...
This dataset has no description
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(Tab 2) Average signal to noise ratio (SNR) for individual microarray probes ...
This dataset has no description
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(Tab 1) Biogeochemistry of groundwater during acetate and bicarbonate amendme...
Sampling port depths are for the depths are in meters below ground surface (BGS) and are for discrete multichannel sampling ports. If no depth is given, wells are typically... -
Macroinvertebrate abundance in montane tropical streams of varying land-use, ...
Despite the importance of tropical montane cloud forest streams, studies investigating aquatic communities in these regions are rare and knowledge on the driving factors of... -
Seismic inversion models and results from the Tuaheni Landslide Complex (New ...
The data files are results of seismic inversions carried out with seismic reflection data from the Tuaheni Landslide Complex, east of New Zealand's North Island on the Hikurangi... -
Seismic horizon interpretations from the Tuaheni Landslide Complex (New Zealand)
These seismic horizon interpretations we made from the seismic reflection data described in https://doi.pangaea.de/10.1594/PANGAEA.927990, using IHS Kingdom Suite software... -
Seismic reflection data from the Tuaheni Landslide Complex (New Zealand)
This dataset includes seismic reflection data from the region of the Tuaheni Landslide Complex, east of New Zealand's North Island on the Hikurangi margin. The seismic... -
(Tables 1-3) Amphipod species observed under Antarctic pack ice during POLARS...
During three Antarctic expeditions (2004, ANT XXI-4 and XXII-2; 2006, ANT XXIII-6) with the German research icebreaker R/V Polarstern, six different amphipod species were... -
(Table 3) Interannual variability of total mass flux at the deep sediment tra...
This article will review major features of the 'giant' Cape Blanc filament off Mauritania with regard to the transport of chlorophyll and organic carbon from the shelf to the... -
(Table 1) Lake elevation change derived from 4 or more years of measurements
In this study, ICESat altimetry data are used to provide precise lake elevations of the Tibetan Plateau (TP) during the period of 2003-2009. Among the 261 lakes examined ICESat... -
(Tables 2-7) Soil characteristics and geochemistry of marshland in the North ...
Results from a large scale soil mapping on the North Frisian mainland indicate, that field characteristics, particularly the grain-size, bedding, and degree of compaction, with... -
(Table 2) Positions of the redox line and the ratio of the thickness of the o...
Sediment temperatures are given in Table 1, see: -
(Table 1) Observations on box cores surfaces taken during Sonne cruise SO95
This dataset has no description
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Elevation measurements and sea level interpretations for South Africa Pliocen...
This dataset has no description
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Scarp points of the Atlantic Coastal Plain between 32° N and 38° N
RSL = relative sea level -
(Table S1) Molecular analyses and morphological comparisons of deep-sea clams
Large vesicomyid clams are common inhabitants of sulphidic deep-sea habitats such as hydrothermal vents, hydrocarbon seeps and whale-falls. Yet, the species- and genus-level... -
Tab. 1: Major cation content McMurdo Dry Valley soils
Matric effects contribute less to the water potential of soils in the McMurdo Dry Valleys of Antarctica (informally known as the Ross Desert) than do the mineral salts of these... -
(Appendix) Petrographic record from excavation profiles in Old-Luebeck (Liubi...
Die Frage einer Küstensenkung spielt seit Jahrzehnten bei der geologischen Erforschung des norddeutschen und niederländischen Flachlandes eine große Rolle. Der Schwerpunkt der...
