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Lithostratigraphic units of IODP Hole 364-M0077A
Determined using Corelyzer. Boundary is defined at the average depth if it is inclined. Bottom of Unit 3B is defined as first occurrence of granitic rocks. -
Daily temperature data from the Foothills Climate Array Mesonet, Canadian Roc...
Near-surface air temperatures were monitored from 2005 to 2010 in a mesoscale network of 230 sites in the foothills of the Rocky Mountains in southwestern Alberta, Canada. The... -
Seismic locations, geochemical variations, attenuation anomalies, geomorpholo...
Despite their importance for eruption forecasting the causes of seismic rupture processes during caldera unrest are still poorly reconstructed from seismic images. Seismic... -
Anthropogenic lead concentrations in Amazonian wildlife and from samples repr...
We analyse lead levels and isotopic fingerprint in 18 free-ranging wild game species in remote areas of the Amazon to provide a comprehensive picture of lead pollution and... -
Cyanobacteria biomass experiment 2012
This dataset has no description
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Supplementary aDNA sequences from a Pleistocene ground squirrel midden, Yukon
Data consists of sequence data of plants and fungi from a Pleistocene ground squirrel midden (collected from a small placer goldmine on Little Blanche Creek, Klondike area near... -
Synthetic data for the Bedforms Analysis Toolkit for Multiscale Modeling (Bed...
Bedforms Analysis Toolkit for Multiscale Modeling (Bedforms-ATM) is an open source MATLAB software which is aimed to standardize the analysis of variability of bed forms.... -
Abundance of planktonic foraminifera from IODP Hole 339-U1386C
The base of the Faro contouritic drift (IODP Site U1386) on the northern margin of the Gulf of Cádiz (Algarve margin) is characterized by two sequences of frequent gravity... -
(Table 2.1) Morphology of the Foundation Seamounts, Sonne cruise SO100
This dataset has no description
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Modeled monthly local topographic lapse rates, Pacific Northwest, USA
An emerging approach to downscaling the projections from General Circulation Models (GCMs) to scales relevant for basin hydrology is to use output of GCMs to force... -
Maps (pdf) and raster images (tif) of predicted rural land cover suitability ...
This study projects land cover probabilities under climate change for corn (maize), soybeans, spring and winter wheat, winter wheat-soybean double cropping, cotton, grassland... -
Physical models of dilatant normal faulting in jointed cohesive rocks
Dilatant faults often form in rocks containing pre-existing joints, but the effects of joints on fault segment linkage and fracture connectivity is not well understood. We... -
Evolution of extreme stomach pH in bilateria inferred from gastric alkalizati...
The stomachs of most vertebrates operate at an acidic pH of 2 generated by the gastric H+/K+-ATPase located in parietal cells. The acidic pH in stomachs of vertebrates is... -
(Table 1) Diagnostic characters of specimens of Marenzelleria bastropi sp. n....
Marenzelleria bastropi, a new species of Spionidae (Polychaeta) from the brackish water Currituck Sound, North Carolina, is described. The new species is characterized by the... -
(Table 1) Organohalogen contaminants in adipose tissue of captive sledge dogs...
Studies on the fate of organohalogen contaminants (OHCs) in wild top predator mammals in the Arctic have often been a challenge due to important knowledge deficiencies in the... -
(Table 2) Survivorship of transplanted seedlings of Picea glauca inside and o...
The northern boundary of boreal forest and the ranges of tree species are expected to shift northward in response to climate warming, which will result in a decrease in the... -
Model results of sensitivity experiments for marine nitrogen cycle in four Ne...
The marine nitrogen (N) inventory is thought to be stabilized by negative feedback mechanisms that reduce N inventory excursions relative to the more slowly overturning... -
(Tabls S1) Bulk geochemistry for sediment samples collected from the Cenomani...
Oceanic Anoxic Event 2 (OAE2), spanning the Cenomanian-Turonian boundary (CTB), represents one of the largest perturbations in the global carbon cycle in the last 100 Myr. The... -
(Table 1) Bulk geochemistry of some lavas at DSDP Hole 55-433C
According to Wilson's (1963a, b) hypothesis, the volcanoes of the Hawaiian-Emperor Chain are formed as the Pacific lithospheric plate moves over a source of magma in the mantle.... -
(Table 1) Isotopes, calcite, aragonite and sample descriptions at DSDP Hole 5...
Calcite in the cavities and veins of igneous rocks has long been recognized as an alteration by-product (Dana, 1892). Elementary mineralogy textbooks report that the most common...
