8,936 Works

Gravity potential spherical harmonic series, supplement to: Gruber, Thomas; Bamber, Jonathan L; Bierkens, Marc F P; Dobslaw, H; Murböck, M; Thomas, M; van Beek, L P H; van Dam, T; Vermeersen, L L A; Visser, P N A M (2011): Simulation of the time-variable gravity field by means of coupled geophysical models. Earth System Science Data, 3(1), 19-35

Thomas Gruber, Jonathan L Bamber, Marc F P Bierkens, H Dobslaw, M Murböck, M Thomas, L P H van Beek, T van Dam, L L A Vermeersen & P N A M Visser
Time variable gravity fields, reflecting variations of mass distribution in the system Earth is one of the key parameters to understand the changing Earth. Mass variations are caused either by redistribution of mass in, on or above the Earth's surface or by geophysical processes in the Earth's interior. The first set of observations of monthly variations of the Earth gravity field was provided by the US/German GRACE satellite mission beginning in 2002. This mission is...

(Table S1) Chronostratigraphic constrains for sediment core AND1-1B, supplement to: Naish, Tim R; Powell, Ross; Levy, Richard H; Wilson, Gary S; Scherer, Reed P; Talarico, Franco M; Krissek, Lawrence A; Niessen, Frank; Pompilio, Massimo; Wilson, Terry; Carter, Lionel; DeConto, Robert M; Huybers, Peter; McKay, Robert M; Pollard, David; Ross, J; Winter, Diane M; Barrett, Peter J; Browne, G; Cody, Rosemary; Cowan, Ellen A; Crampton, James; Dunbar, Gavin B; Dunbar, Nelia W; Florindo, Fabio; Gebhardt, Catalina; Graham, I J; Hannah, Mike J; Hansaraj, D; Harwood, David M; Helling, D; Henrys, Stuart A; Hinnov, Linda A; Kuhn, Gerhard; Kyle, Philip R; Läufer, Andreas L; Maffioli, P; Magens, Diana; Mandernack, Kevin W; McIntosh, W C; Millan, C; Morin, Roger H; Ohneiser, Christian; Paulsen, Timothy S; Persico, Davide; Raine, J Ian; Reed, J; Riesselman, Christina R; Sagnotti, Leonardo; Schmitt, Douglas R; Sjunneskog, Charlotte; Strong, P; Taviani, Marco; Vogel, Stefan; Wilch, T; Williams, Trevor (2009): Obliquity-paced Pliocene West Antarctic ice sheet oscillations. Nature, 458(7236), 322-329

Tim R Naish, Ross Powell, Richard H Levy, Gary S Wilson, Reed P Scherer, Franco M Talarico, Lawrence A Krissek, Frank Niessen, Massimo Pompilio, Terry Wilson, Lionel Carter, Robert M DeConto, Peter Huybers, Robert M McKay, David Pollard, J Ross, Diane M Winter, Peter J Barrett, G Browne, Rosemary Cody, Ellen A Cowan, James Crampton, Gavin B Dunbar, Nelia W Dunbar, Fabio Florindo … & Trevor Williams
Thirty years after oxygen isotope records from microfossils deposited in ocean sediments confirmed the hypothesis that variations in the Earth's orbital geometry control the ice ages (Hays et al., 1976, doi:10.1126/science.194.4270.1121), fundamental questions remain over the response of the Antarctic ice sheets to orbital cycles (Raymo and Huybers, 2008, doi:10.1038/nature06589). Furthermore, an understanding of the behaviour of the marine-based West Antarctic ice sheet (WAIS) during the 'warmer-than-present' early-Pliocene epoch (~5-3 Myr ago) is needed to...

Downhole logging of the AND-2A borehole, Victoria Land Basin, McMurdo Sound, Antarctica, supplement to: Wonik, Thomas; Grelle, Thomas; Handwerger, David A; Jarrard, Richard D; McKee, Andrew; Patterson, Taylor; Paulsen, Timothy S; Pierdominici, Simona; Schmitt, Douglas R; Schröder, Henning; Speece, Marvin; Wilson, Terry; SMS Science Team (2009): Downhole measurements in the AND-2A borehole, ANDRILL southern McMurdo Sound Project, Antarctica. Terra Antartica, 15(1), 41-48

Thomas Wonik, Thomas Grelle, David A Handwerger, Richard D Jarrard, Andrew McKee, Taylor Patterson, Timothy S Paulsen, Simona Pierdominici, Douglas R Schmitt, Henning Schröder, Marvin Speece, Terry Wilson & SMS Science Team
Under the framework of the ANDRILL Southern McMurdo Sound (SMS) Project successful downhole experiments were conducted in the 1138.54 metre (m)-deep AND-2A borehole. Wireline logs successfully recorded were: magnetic susceptibility, spectral gamma ray, sonic velocity, borehole televiewer, neutron porosity, density, calliper, geochemistry, temperature and dipmeter. A resistivity tool and its backup both failed to operate, thus resistivity data were not collected. Due to hole conditions, logs were collected in several passes from the total depth...

(Table S1) Age determination of sediment cores GeoB1720-3 and GeoB1720-2

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost

Seawater carbonate chemistry and calcification of Lophelia pertusa during experiments, 2009, supplement to: Maier, Cornelia; Hegeman, Jan; Weinbauer, Markus G; Gattuso, Jean-Pierre (2009): Calcification of the cold-water coral Lophelia pertusa under ambient and reduced pH. Biogeosciences, 6(8), 1671-1680

Cornelia Maier, Jan Hegeman, Markus G Weinbauer & Jean-Pierre Gattuso
The cold-water coral Lophelia pertusa is one of the few species able to build reef-like structures and a 3-dimensional coral framework in the deep oceans. Furthermore, deep cold-water coral bioherms may be among the first marine ecosystems to be affected by ocean acidification. Colonies of L. pertusa were collected during a cruise in 2006 to cold-water coral bioherms of the Mingulay reef complex (Hebrides, North Atlantic). Shortly after sample collection onboard these corals were labelled...

Stable isotope record and aklenonen index of MIS 11 sediments, supplement to: Dickson, Alexander J; Beer, Christopher J; Dempsey, Ciara; Maslin, Mark A; Bendle, James A; McClymont, Erin L; Pancost, Richard D (2009): Oceanic forcing of the Marine Isotope Stage 11 interglacial. Nature Geoscience, 2, 428-433

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost
The interglacial known as Marine Isotope Stage 11 has been proposed to be analogous to the Holocene, owing to similarities in the amplitudes of orbital forcing. It has been difficult to compare the periods, however, because of the long duration of Stage 11 and a lack of detailed knowledge of any extreme climate events that may have occurred. Here we use the distinctive phasing between seasurface temperatures and the oxygen-isotope records of benthic foraminifera in...

(Table S3) Stable isotope ratios of Cibicidoides wuellerstorfi sediment cores GeoB1720-3

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost

(Table S6) UK'37 index and sea surface temperature reconstruction of ODP Site 175-1085

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost

(Table S2) Stable isotope ratios of Cibicidoides wuellerstorfi of sediment cores GeoB1720-2

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost

(Table S4) UK'37 index and sea surface temperature reconstruction of sediment cores GeoB1720-2

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost

(Table S5) UK'37 index and sea surface temperature reconstruction of sediment cores GeoB1720-3

Alexander J Dickson, Christopher J Beer, Ciara Dempsey, Mark A Maslin, James A Bendle, Erin L McClymont & Richard D Pancost

Paleomagnetic of the Eocene and Oligocene section of ODP Hole 151-913B

James S Eldrett, Ian C Harding, Paul A Wilson, Emily Butler & Andrew P Roberts

(Fig 5) Geochemistry and rock magnetic parameters of sediment cores K2, K3, K5

Hendrik Müller, Tilo von Dobeneck, Wiebke Nehmiz & Kay Hamer

Vertical microalgae fluxes at the mooring station LOMO-2 over the Lomonosov Ridge in the period from September 15, 1995 till August 16, 1996, supplement to: Zernova, Valentina V; Nöthig, Eva-Maria; Shevchenko, Vladimir P (2000): Vertical microalga flux in the northern Laptev Sea (from the data collected by the yearlong sediment trap). Translated from Okeanologiya, 2000, 40(6), 850-858, Oceanology, 40(6), 801-808

Valentina V Zernova, Eva-Maria Nöthig & Vladimir P Shevchenko
The first studies of microalgae fluxes over the Lomonosov Ridge in the northern Laptev Sea were carried out with a sediment trap at the year-long mooring station LOMO-2, installed at 150 m depth from September 15, 1995 to August 16, 1996. These studies demonstrated essential seasonal variations of vertical microalgae flux. It was shown that in summer diverse flora (composed mainly of cryophylic diatoms) growed intensively beneath the permanent ice cover. Strongly pronounced seasonal variations...

(Table 6a) 137Cs concentrations in waters of the Sea of Japan in 1994 and in 2002

Mikhail M Domanov, V V Kobylyansky, A I Svininnikov, Elena G Vodyanaya, M V Vladimirov & Oleg L Kuznetsov
Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along...

(Table 6b) 137Cs concentrations in surface layer bottom sediments of the Sea of Japan in 1994 and in 2002

Mikhail M Domanov, V V Kobylyansky, A I Svininnikov, Elena G Vodyanaya, M V Vladimirov & Oleg L Kuznetsov
Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along...

Reference list of sources used for two experimental data files dataBSRN and dataMixed

Maximilian Scherer, Jürgen Bernard & Tobias Schreck
Increasing amounts of data is collected in most areas of research and application. The degree to which this data can be accessed, analyzed, and retrieved, is a decisive in obtaining progress in fields such as scientific research or industrial production. We present a novel methodology supporting content-based retrieval and exploratory search in repositories of multivariate research data. In particular, our methods are able to describe two-dimensional functional dependencies in research data, e.g. the relationship between...

(Table 3) Recalculated lead isotope ratios of ODP Leg 125 rock samples

Julian A Pearce, Matthew F Thirlwall, Gerry Ingram, Bramley J Murton, Richard J Arculus & Sieger R van der Laan
Recalculated = alteration corrected. The assumed metamorphic age is given as age model if it differs from the magmatic age (= AGE).

(Table 4) Analyses of titanomagnetite of ODP Hole 125-781A

Michael S Marlow, Lynn E Johnson, Julian A Pearce, Patricia B Fryer, Ledabeth G Pickthorn & Bramley J Murton

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