24,013 Works

Characterizing Shape Using Conformal Factors

Mirela Ben-Chen & Craig Gotsman
Eurographics 2008 Workshop on 3D Object Retrieval
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Aeolian dust and chemistry record of ice core EDML

Urs Ruth
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Pollen analysis of ODP Hole 175-1078C (part 1), counts of total pollen and fern spores

Lydie M Dupont, Hermann Behling & Jung-Hyun Kim
Depth=depth composit
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AMS radiocarbon dates of ODP Hole 175-1078C below 9.80 mbsf

Lydie M Dupont, Hermann Behling & Jung-Hyun Kim
Calibration using R=400 after Fairbanks et al. (2005).
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Pollen analysis of ODP Hole 175-1078C (part 2), counts of total pollen and fern spores

Lydie M Dupont, Hermann Behling & Jung-Hyun Kim
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Rare earth elements determined in ice core EDML by laser-ablation inductively coupled plasma quadrupole mass spectrometry (La-ICP-Q-MS) in 269-270 m depth

Dorothee Dick & Michael Kriews
Only values exceeding the DL and the lowest concentrated standard are shown.
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Aeolian dust and chemistry record of ice core EDC

Urs Ruth
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Chemistry on ice core VEF81

A V Korsun, A V Evseyev, S A Korsun, Ya-M K Punning & V S Zagorodnov
including unpublished data/personal communication of Golubev, V N; Vaikmaye, R A
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Multi-GPU Sort-Last Volume Visualization

Stéphane Marchesin, Catherine Mongenet & Jean-Michel Dischler
Eurographics Symposium on Parallel Graphics and Visualization
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Paleorecords from MD02-2575 (Figure 2), supplement to: Ziegler, Martin; Nürnberg, Dirk; Karas, Cyrus; Tiedemann, Ralf; Lourens, Lucas Joost (2008): Persistent summer expansion of the Atlantic Warm Pool during glacial abrupt cold events. Nature Geoscience, 1, 601-605

Martin Ziegler, Dirk Nürnberg, Cyrus Karas, Ralf Tiedemann & Lucas Joost Lourens
Palaeoclimate records and numerical model simulations indicate that changes in tropical and subtropical sea surface temperatures and in the annual average position of the intertropical convergence zone are linked to high-latitude climate changes on millennial to glacial-interglacial timescales. It has recently been suggested that cooling in the high latitudes associated with abrupt climate-change events is evident primarily during the northern hemisphere winter, implying increased seasonality at these times. However, it is unclear whether such a...
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Ozone measurements from station Boulder (2002-02)

Ellsworth G Dutton
Location: Boulder, Colorado, USA; Distance from radiation site: 16 km
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Trawlings during VOZROZHDENIE cruise VOZ1

Sergey Piontkovski & A R Boltachev
The fish catches were carried out by the industrial midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 6.5 mm in the trawl bag. Vertical opening of the trawl made from 30 to 50 m. The trawling duration under catches in the sound-scattering layers made 1-2 hour, under fish schools catches - from 15 min to 2 hours. Speed of trawling made 3.2-4.2 knots. The catches horizons were determined by the...
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Trawlings during TITANIT cruise TIT1, Part II

Sergey Piontkovski & A R Boltachev
The fish catches were carried out by the industrial midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 6.5 mm in the trawl bag. Vertical opening of the trawl made from 26 to 42 m. The trawling duration under catches in the sound-scattering layers made 1 hour, under fish schools catches - from 40 min up to 2 hours and 20 min. Speed of trawling made 3.2-4.2 knots. The catches horizons...
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Trawling of fish during ALKOR cruise AL220/1

Rüdiger Voss & Axel Temming
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Trawlings during Professor Vodyanitskiy cruise PV24, Part II

Sergey Piontkovski & A R Boltachev
The fish catches were carried out by the scientific midwater non-closed trawl. There was a small-mesh section with minimum mesh size of 0.11-0.07 mm in the trawl bag. Vertical opening of the trawl made up to 6 m. The trawling duration under catches in the sound-scattering layers made 30 min. Speed of trawling made 3.0 knots. The trawling survey has been carried out in the Equatorial zone along 6°, 12°, 18° and 24° W meridians...
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Tree-ring width of Quercus species from historical object sample HOF10017-4

Jutta Hofmann
Species QUSP; No of rings 56; Begin 1556; End 1611
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(Appendix A) Methane and helium isotope data in water profile M62/5b-1226-CTD-LADCP

Robin Keir, Oliver Schmale, Maren Walter, Jürgen Sültenfuß, Richard Seifert & Monika Rhein
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Sea surface salinity reconstructed from sediment core SO93-126KL

Hermann-Rudolph Kudrass, Annette Hofmann, Heidi Doose, Kay-Christian Emeis & Helmut Erlenkeuser
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(Table 2) Barium concentrations of surface sediments in the Mediterranean Sea

Syee Weldeab, Kay-Christian Emeis, Christoph Hemleben, Gerhard Schmiedl & Hartmut Schulz
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Geochemistry of sediments cores in the Mediterranean Sea, supplement to: Weldeab, Syee; Emeis, Kay-Christian; Hemleben, Christoph; Schmiedl, Gerhard; Schulz, Hartmut (2003): Spatial productivity variations during formation of sapropels S5 and S6 in the Mediterranean Sea: Evidence from Ba contents. Palaeogeography, Palaeoclimatology, Palaeoecology, 191(2), 169-190

Syee Weldeab, Kay-Christian Emeis, Christoph Hemleben, Gerhard Schmiedl & Hartmut Schulz
We investigated five time-equivalent core sections (180-110 kyr BP) from the Balearic Sea (Menorca Rise), the easternmost Levantine Basin and southwest, south, and southeast of Crete to reconstruct spatial patterns of productivity during deposition of sapropels S5 and S6 in the Mediterranean Sea. Our indicators are Ba, total organic carbon and carbonate contents. We found no indications of Ba remobilization within the investigated core intervals, and used the accumulation rate of biogenic Ba to compute...
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(Table 4) Occurrence of sapropels and marker layers in ODP Site 160-969 in the eastern Mediterranean Sea

Kay-Christian Emeis, Tatsuhiko Sakamoto, Rolf Wehausen & Hans-Jürgen Brumsack
Depth is the midpoint of the sediment interval
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(Table 1) Occurrence of sapropels and marker layers in ODP Site 160-964 in the eastern Mediterranean Sea

Kay-Christian Emeis, Tatsuhiko Sakamoto, Rolf Wehausen & Hans-Jürgen Brumsack
Depth is the midpoint of the sediment interval
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(Table 3) Occurrence of sapropels and marker layers in ODP Site 160-967 in the eastern Mediterranean Sea

Kay-Christian Emeis, Tatsuhiko Sakamoto, Rolf Wehausen & Hans-Jürgen Brumsack
Depth is the midpoint of the sediment interval
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(Table 2) Occurrence of sapropels and marker layers in ODP Site 160-966 in the eastern Mediterranean Sea

Kay-Christian Emeis, Tatsuhiko Sakamoto, Rolf Wehausen & Hans-Jürgen Brumsack
Depth is the midpoint of the sediment interval
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The sapropel record of the eastern Mediterranean Sea, supplement to: Emeis, Kay-Christian; Sakamoto, Tatsuhiko; Wehausen, Rolf; Brumsack, Hans-Jürgen (2000): The sapropel record of the eastern Mediterranean Sea - results of Ocean Drilling Program Leg 160. Palaeogeography, Palaeoclimatology, Palaeoecology, 158(3-4), 371-395

Kay-Christian Emeis, Tatsuhiko Sakamoto, Rolf Wehausen & Hans-Jürgen Brumsack
Research on sediments recovered during Ocean Drilling Leg 160 has concentrated on two issues: the first concerned the stratigraphy of sapropel formation, the second was oriented to clarify specific processes that explain sapropel origin. Progress has been made in the construction of stratigraphic composites out of sedimentary sequences from individual holes at each of the palaeoceanographic sites. On the composites, initial work has resulted in the establishment of high-resolution and intermediate-resolution stratigraphies for three sites...
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