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Geostatistical analyses of IODP Hole 339-U1386B
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1386A
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1389D
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Geostatistical analyses of IODP Hole 339-U1389C
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging... -
Soil organic carbon (SOC) and sediment contents and fluxes for terrain units ...
Narrowing uncertainties about carbon cycling is important in the Arctic where rapid environmental changes contribute to enhanced mobilization of carbon. Here we quantify soil... -
(Table 3) Components of the short wave radiation investigated during Atlantic...
Lambda max = 684 nm. Altitude is a rough estimate from pressure. -
(Table 3) Components of the short wave radiation investigated during Atlantic...
Lambda max = 684 nm. Altitude is a rough estimate from pressure. -
(Table 3) Components of the short wave radiation investigated during Atlantic...
Lambda max = 684 nm. Altitude is a rough estimate from pressure. -
(Table 2) Components of the short wave radiation investigated during Atlantic...
Lambda max = 550 nm. Altitude is a rough estimate from pressure. -
(Table 2) Components of the short wave radiation investigated during Atlantic...
Lambda max = 550 nm. Altitude is a rough estimate from pressure. -
(Table 2) Components of the short wave radiation investigated during Atlantic...
Lambda max = 550 nm. Altitude is a rough estimate from pressure. -
Vertical day-night distribution of the salp Soestia zonaria in the temperate ...
Although the oceanic widespread pelagic tunicate Soestia zonaria has been studied for more than a century, little ecological information exists. Soestia primarily occurs in... -
(Table 3) Age-related trends of desert pavement properties in the Transantarc...
Compared to mid-latitude deserts, the properties, formation and evolution of desert pavements and the underlying vesicular layer in Antarctica are poorly understood. This study... -
(Table 2) Soil properties and soil chemistry under forest, sub-páramo and pas...
This dataset has no description
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(Table 22) Vegetation, soil and site characteristics of all relevés sampled a...
Mean thaw depths for relevees 40 through 44 are given as NSC/Inter -
(Table A1) Bottom layer properties during Nathanial B. Palmer cruise NBP00-08...
Dissolved oxygen was originally given in ml/l and was recalculated to µmol/l by multiplying by 44.66; Definition of concentration at bottom and accross bottom layer thickness... -
(Table A2) Bottom layer properties during Nathanial B. Palmer cruise NBP04-08...
Dissolved oxygen was originally given in ml/l and was recalculated to µmol/l by multiplying by 44.66; Definition of concentration at bottom and accross bottom layer thickness... -
(Table 1) Thickness of Layer 1 of Fe-Mn crusts at seamounts in the Northwest ...
This dataset has no description
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(Table 1) Composition of upper Quaternary sediments from ODP Hole 127-797B
This dataset has no description
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(Table 1) Structural and textural characteristics of the turbiditic sequence ...
This dataset has no description
