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Benthic foraminifera abundance of sediment core MD01-2416
This dataset has no description
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Planktic foraminifera abundance and ecological groups of Hole PRAD1-2
This dataset has no description
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(Table 1) Detrital modes for sand grains in sediment core CRP-2/2A
Dynamic provenance variations are deduced from sand-grain detrital modes in samples obtained from the CRP-2/2A drillcore. Below an important unconformity at 307 metres below sea... -
Phytoplankton biomass from the Namibian upwelling system duringMETEOR cruise ...
Phytoplankton data from the cruise number M103-2 with research vessel "Meteor" from 20.1.2014 to 11.2.2014 (from Walvis Bay to Walvis Bay) in front of Namibia. Phytoplankton... -
Phytoplankton biomass from the Namibian upwelling system during METEOR cruise...
Phytoplankton data from the cruise number M103-1 with research vessel "Meteor" from 27.12.2013 to 18.1.2014 (from Walvis Bay to Walvis Bay) in front of Namibia. Phytoplankton... -
Phytoplankton biomass from the Namibian upwelling system during Maria S. Mera...
Geocode DEPTH, water is the mid depth of the range. Phytoplankton counted by means of inverted microscope according to the classical UTERMÖHL method. Counts converted to biomass... -
Planktic foraminifera counts of sediment core V20-242
This dataset has no description
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Planktic foraminifera counts of sediment core V20-175
This dataset has no description
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Planktic foraminifera counts of sediment core V20-170
This dataset has no description
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Mineralogical analysis by X-Ray diffraction of Hashilan Wetland sediment core...
For mineralogical analysis by X-Ray Diffraction (XRD), samples of ~ 1 gram were dried at 50 °C for 48 hours. The dried samples were ground and homogenized using mortar and... -
Concentration of the most abundant planktonic foraminifera species collected ...
This dataset has no description
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XRD analyses of core Konar Sandal peat bog, SE Iran
This dataset has no description
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Time series of phytoplankton abundance and composition at station L4 in the E...
Weekly phytoplankton samples are collected from station L4 (50°15.00'N 4°13.02'W) in the western English Channel http://www.westernchannelobservatory.org.uk/l4/Phytoplankton... -
Time series of microzooplankton abundance and composition at station L4 in th...
Weekly microzooplankton samples are collected from station L4 (50°15.00'N 4°13.02'W) in the western English Channel http://www.westernchannelobservatory.org.uk/l4/Phytoplankton... -
(Table 2) Benthic foraminiferal numbers and species abundance of sediment cor...
Age model after Kido et al. (2007, doi:10.1016/j.palaeo.2006.11.020) and Yokoyama et al. (2007, doi:10.1016/j.palaeo.2006.11.018) -
(Table 1) Planktonic foraminiferal numbers and species abundance in sediment ...
Age model after Kido et al. (2007, doi:10.1016/j.palaeo.2006.11.020) and Yokoyama et al. (2007, doi:10.1016/j.palaeo.2006.11.018). For several samples planktonic foraminiferal... -
Mean abundances of epigeic arthropods on Mount Kilimanjaro
On each site, ten pitfall traps were evenly spaced along two 50 m transects, with a distance of 10 m between individual traps and 20 m between transects. Pitfall traps were... -
Nannoliths content of MIRA-CP1 core, Portugal
Sixteen calcareous nannoplankton taxa and didemnid ascidian spicules were identified throughout MIRA-CP1 core (see Alday et al. 2006 for further details). On the basis of... -
Dirac Nodal Line Magnons in a Stacked Honeycomb Magnet
On the basis of exchange couplings obtained from early inelastic neutron measurements, we conjecture that the stacked honeycomb magnet FeTiO3 contains Dirac nodal lines in the... -
Neutron scattering study of a triangular-lattice NaYbO2: a quantum spin liqui...
The Quantum spin liquid (QSL) state continues to fascinate the condensed matter community. This is because the spins in a QSL are highly entangled and fluctuate strongly down to...
