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Abstract: This dataset contains raster grids in GeoTIFF format describing the constraints on accumulation of tropical peat imposed by drainage network geometry in regions of northwest and southern Borneo. Each raster in the dataset gives the geometric capacity for peat accumulation (non-dimensional equilibrium peat thickness) in a parcel of land, calculated using the method described in the paper. The parcels are grouped into five areas, referred to by the names Badas, Baram, Belait, EMRP and Sebangau. Rasters have arbitrary numeric labels (001.tif, 002.tif, ...) in all areas except the Badas area, where descriptive names are used for the parcels before (badas) and after (badas_west and badas_east) subdivision by a canal. The map projection and resolution are included in each raster via standard GeoTIFF metadata; the projections used were EPSG:5247 for the Badas, Baram, and Belait areas and EPSG:32749 for the EMRP and Sebangau areas. Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: Not Available
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Abstract: Not Available Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: EVENT LABEL: * LATITUDE START: 4.453500 * LONGITUDE START: 114.284800 * LATITUDE END: 4.643700 * LONGITUDE END: 114.454800 * METHOD/DEVICE: Multiple investigations
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Abstract: Not Available Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: EVENT LABEL: * LATITUDE START: 4.393100 * LONGITUDE START: 114.278400 * LATITUDE END: 4.409500 * LONGITUDE END: 114.297100 * METHOD/DEVICE: Multiple investigations
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Abstract: Not Available Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: EVENT LABEL: * LATITUDE START: 4.256200 * LONGITUDE START: 114.304100 * LATITUDE END: 4.550000 * LONGITUDE END: 114.468300 * METHOD/DEVICE: Multiple investigations
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Abstract: Not Available Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: EVENT LABEL: * LATITUDE START: -2.465800 * LONGITUDE START: 114.415900 * LATITUDE END: -2.232100 * LONGITUDE END: 114.565600 * METHOD/DEVICE: Multiple investigations
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Abstract: Not Available Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: Not Available
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Abstract: Not Available Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: EVENT LABEL: * LATITUDE START: -3.014900 * LONGITUDE START: 113.031500 * LATITUDE END: -1.951000 * LONGITUDE END: 114.052500 * METHOD/DEVICE: Multiple investigations
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Abstract: 1-Hz displacements at GEONET (GPS Earth Observation Network) stations in Japan during the 2011 Tohoku Mw9.0 earthquake. The displacements were obtained using the method of Precise Point Positioning with the PANDA software. Totally 1221 stations are included, spanning from 14:45 to 15:30 on March 11, 2011 in Japan local time. Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: Not Available
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Abstract: The data set contains 5-min resolution meteorological data (temperature and relative humidity), 5-min resolution isotopic composition of water vapor, isotopic composition of precipitation for 11 rain events, isotopic composition of 10 river samples, isotopic composition of 6 leaf water samples and isotopic composition of 5 cellulose samples. The data are in February and March 2017. The site location is 41°47.412'S, 71°34.355'W, 1175 m. Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: Not Available
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Abstract: Ravine slopes at the recently discovered Nesseltalgraben site in southeastern Germany provide a unique last glacial sediment record for the Northern Calcareous Alps. The 21 m-long profile is dominated by fine-grained lacustrine-palustrine sediments overlain by several metres of glacifluvial gravels and lodgement tills of the Last Glacial Maximum and underlain by a diamicton. The age model includes 29 radiocarbon analyses and one paleomagnetic anomaly (Laschamp event) together providing a modelled age range from c. 59 to 29.6 ka cal BP, i.e. Marine Isotope Stage (MIS) 3. Apart from a description of the lithofacies, X-ray-fluorescence (XRF) scanning and elemental analyses provide high-resolution records of the geochemical composition. Multivariate analyses of XRF data separate Ca from other major elements. Carbonate contents, represented by Ca and total inorganic carbon, reach maxima in repeatedly occurring calcareous silty to sandy layers and are related to glacigenic origin. These indicate repeated inner-alpine local glaciations during stadials of MIS 3. Scanning electron microscopy and XRF data confirm the detrital origin of these layers. In contrast, organic matter and elements more resistant to chemical weathering (Si, Ti, Zr) accumulated during interstadials and concurrently elevated Rb/Sr ratios indicate intensified weathering. The high-frequency proxy variations determined for Nesseltalgraben reflect interstadial-stadial climate variability comparable with oxygen-isotope records from Greenland ice cores and Alpine speleothems. Thus, Nesseltalgraben is among the very few independently dated sediment records from continental Europe covering the entire MIS 3 and reflecting the full Dansgaard-Oeschger climate variability. Category: geoscientificInformation Source: Not Available Supplemental Information: Not Availble Coverage: Not Available
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