331,479 Works

Sea surface temperature and export production reconstructions of sediment core MD95-2040

Emilia Salgueiro, Antje H L Voelker, Lucia de Abreu, Fatima F Abrantes, Helge Meggers & Gerold Wefer

Aerosol measurements at station Ny-Ålesund in 2000, raw data

Andreas Herber
for KFM values see doi:10.1594/PANGAEA.743342

Aerosol measurements at station Ny-Ålesund in 2002, raw data

Andreas Herber
for KFM values see doi:10.1594/PANGAEA.743342

Aerosol measurements at station Ny-Ålesund in 2005, raw data

Andreas Herber
for KFM values see doi:10.1594/PANGAEA.743342

Aerosol measurements at station Ny-Ålesund in 2006, raw data

Andreas Herber
for KFM values see doi:10.1594/PANGAEA.743342

Aerosol measurements at station Ny-Ålesund in 2008, raw data

Andreas Herber
for KFM values see doi:10.1594/PANGAEA.743342

Aerosol measurements at station Ny-Ålesund in 2009, raw data

Andreas Herber
for KFM values see doi:10.1594/PANGAEA.743342

XRF element scanning on composite core JH05

Stefan Lauterbach, Achim Brauer, Nils Andersen, Dan L Danielopol, Peter Dulski, Matthias Hüls, Krystyna Milecka, Tadeusz Namiotko, Birgit Plessen, Ulrich von Grafenstein &

Fig. 3. Three parallel δ¹⁸O measurements on summer layers of ten individual varves

Clara Mangili, Birgit Plessen, Christian Wolff & Achim Brauer

Fig. 4c. 2 years varve resolution at the end of PMO

Clara Mangili, Birgit Plessen, Christian Wolff & Achim Brauer

(Figure 5) Range chart of selected dinocysts and acritarchs of ODP Hole 104-642A

Peta J Mudie
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present

(Figure 6) Range chart of selected dinocysts and acritarchs of ODP Hole 104-642C

Peta J Mudie
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present

(Figure 7) Range chart of selected dinocysts and acritarchs of ODP Hole 104-643A

Peta J Mudie
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present

Bacteria at time series station Helgoland Roads, North Sea, in 1968

Gunnar Gerdts

(Table 10) Trace element contents in pyroxenites and gabbroids

Sergey G Skolotnev, Sergey M Lyapunov & Vladimir A Simonov
X-ray fluorescence analyses have been carried out in the Bronnizy expedition IMGRE under leadership of S.M. Lyapunov.

(Table 11) Composition of clino- and orthopyroxenes

Sergey G Skolotnev, Sergey M Lyapunov & Vladimir A Simonov
Analyses have been carried out in the Borok Geophysical Observatory (Institute of Earth Physics, USSR Acad. Sci.).

(Table 14) Chemical composition of harzburgites from the Cape Verde fault

Alexander A Peyve & S A Shcherbakov
Analyses have been carried out in the Bronnizy expedition IMGRE.

(Table 15) Chemical composition of olivines from harzburgites of the Cape Verde fault

Alexander A Peyve & S A Shcherbakov
Analyses have been carried out in the Institute of Earth Physics, USSR Acad. Sci.

(Table 22) Petrophysical properties of rocks from the Cape Verde fault zone

Yury N Raznitsin & L I Zvyagintsev

(Table 4) Composition of basalts from Polygons II and III

Alexander A Peyve & Sergey M Lyapunov

(Table 2b) Stable carbon and oxygen isotope ratios of Globigerina bulloides from sediment core ELT45.029-PC

William R Howard & Warren L Prell

(Table 2d) Stable carbon and oxygen isotope ratios of Globigerina bulloides from sediment core ELT49.017-PC

William R Howard & Warren L Prell

(Table 1) Representative microprobe analyses of minerals from basalts of the Northern and Central blocks, the Amirante Arc

V T Sedin, I A Tatarin & Z G Badredinov
1, 2, and 3 = different crystals in a sample.

(Table 6) Faunal dissimilarity and sea surface temperture estimates for sediment core ELT49.018-PC

William R Howard & Warren L Prell

(Table 6) Faunal dissimilarity and sea surface temperture estimates for sediment core ELT49.023-PC

William R Howard & Warren L Prell

Registration Year

  • 2010
    331,479

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Affiliations

  • North Carolina State University
    11
  • Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences
    7
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    6
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    5
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    5
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    5
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    4
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