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Core overview images (pdf) of IODP Hole 381-M0078B

IODP Expedition 381 Scientists

Carbon isotopic composition and carbonate content of bulk sediment from ODP Hole 198-1209A

Dustin T Harper, Richard E Zeebe, Bärbel Hönisch, Cindy D Schrader, Lucas Joost Lourens & James C Zachos

Vertical core offset (affine table) form different Holes of IODP Site 342-U1410

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike

Oxygen isotopic composition of benthic foraminifer N. truempyi from ODP Hole 198-1209A

Dustin T Harper, Richard E Zeebe, Bärbel Hönisch, Cindy D Schrader, Lucas Joost Lourens & James C Zachos

Carbon and oxygen isotopic composition and Mg/Ca ratio of planktic foraminifer A. soldadoensis from ODP Hole 208-1265A

Dustin T Harper, Richard E Zeebe, Bärbel Hönisch, Cindy D Schrader, Lucas Joost Lourens & James C Zachos

Splice tie points form IODP Site 342-U1410

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike

Carbon and oxygen isotopic composition and Mg/Ca ratio of planktic foraminifer A. soldadoensis from ODP Hole 198-1209A

Dustin T Harper, Richard E Zeebe, Bärbel Hönisch, Cindy D Schrader, Lucas Joost Lourens & James C Zachos

AMSR-E winter snow depth on Arctic sea ice, Version 1.0 (NetCDF) (2002 to 2011), supplement to: Rostosky, Philip; Spreen, Gunnar; Farrell, Sinead L; Frost, Torben; Heygster, Georg; Melsheimer, Christian (2018): Snow Depth Retrieval on Arctic Sea Ice From Passive Microwave Radiometers - Improvements and Extensions to Multiyear Ice Using Lower Frequencies. Journal of Geophysical Research: Oceans, 123(10), 7120-7138

Philip Rostosky, Christian Melsheimer & Gunnar Spreen
The AMSR-E snow depth on Arctic sea ice product contains daily gridded snow depth data for the period from 2002 to 2011 (see also: AMSR-2 snow depth on Arctic sea ice product (2012 to 2018), doi:10.1594/PANGAEA.902747). The product is based on an empirical algorithm using passive microwave satellite observations from the AMSR-E (Advanced Microwave Scanning Radiometer for EOS) sensors on the NASA Aqua satellite, gridded on a polar stereographic grid (EPSG code 3411, Arctic) with...

COSMOS model middle Eocene sensitivity tests with different obliquity values and Greenland-Scotland Ridge depths

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike
Here we publish simulated middle Eocene (43.5-46 Ma) boreal winter sea surface temperature, sea surface salinity as well as mixed layer depth for obliquity minimum and maximum simulation with Greenland-Scotland Ridge (GSR) depth of 500 m. Furthermore, we include annual mean global meridional overturning circulation and current velocities for both orbital configurations and GSR = 500 m and additionally for minimum obliquity and GSR = 200 m. The CO2 level is set to 840 ppm...

(Supplementary Tabel 3) Calcium/Iron ratios and adjusted depth of IODP Hole 342-U1410B

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike

Fatty acid contents for the diatom Conticribra weissflogii

Rita Melo Franco-Santos, Holger Auel, Maarten Boersma, Marleen De Troch, Martin Graeve, Cédric L Meunier & Barbara Niehoff
The larvae of the reef-building polychaete Lanice conchilega can make up to 15% of the summer zooplankton biomass in the North Sea. Despite their importance for reef maintenance (which positively affects the benthic community), little is known about the trophic ecology of this meroplanktonic larva. Qualitative and quantitative estimates of carbon (C) transfer between trophic levels and of fatty acid (FA)-specific assimilation, biosynthesis, and bioconversion can be obtained by compound-specific stable isotope analysis of FA....

(Supplementary Tabel 4) Stable carbon and oxygen isotope data of Nuttallides truempyi at IODP Site 342-U1410

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike

Carbon and nitrogen contents for the diatom Conticribra weissflogii

Rita Melo Franco-Santos, Holger Auel, Maarten Boersma, Marleen De Troch, Martin Graeve, Cédric L Meunier & Barbara Niehoff
The larvae of the reef-building polychaete Lanice conchilega can make up to 15% of the summer zooplankton biomass in the North Sea. Despite their importance for reef maintenance (which positively affects the benthic community), little is known about the trophic ecology of this meroplanktonic larva. Qualitative and quantitative estimates of carbon (C) transfer between trophic levels and of fatty acid (FA)-specific assimilation, biosynthesis, and bioconversion can be obtained by compound-specific stable isotope analysis of FA....

(Supplementary Tabel 3) Calcium/Iron ratios and adjusted depth of IODP Hole 342-U1410A

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike

(Table S1) Representative geochemistry of metamorphic phases from IODP Exp366 samples

Elmar Albers, Wolfgang Bach, Frieder Klein, C D Menzies, Friedrich Lucassen & Damon A H Teagle
Cations pfu calculated on the basis of 6 O for Cpx, 14 O for Chl, 11 O for Prh, 12 O for Pmp, 11 O for Ph, 8 O for Lws, 23 O for Gln.Abbreviations: Chl, chlorite; Cpx, clinopyroxene; Gln, glaucophane; Lws, lawsonite; pfu, per formula unit; Ph, phengite; Pmp, pumpellyite; Prh, prehnite.

(Table 3) Carbonate and sulfate Sr and stable isotope geochemistry of IODP Exp366 samples

Elmar Albers, Wolfgang Bach, Frieder Klein, C D Menzies, Friedrich Lucassen & Damon A H Teagle

AMSR-2 winter snow depth on Arctic sea ice, Version 1.0 (NetCDF) (2012 to 2018), supplement to: Rostosky, Philip; Spreen, Gunnar; Farrell, Sinead L; Frost, Torben; Heygster, Georg; Melsheimer, Christian (2018): Snow Depth Retrieval on Arctic Sea Ice From Passive Microwave Radiometers - Improvements and Extensions to Multiyear Ice Using Lower Frequencies. Journal of Geophysical Research: Oceans, 123(10), 7120-7138

Philip Rostosky, Christian Melsheimer & Gunnar Spreen
The AMSR-2 snow depth on Arctic sea ice product contains daily gridded snow depth data for the period from 2012 to 2018 (see also: AMSR-E snow depth on Arctic sea ice product (2002 to 2011), doi:10.1594/PANGAEA.902748). The product is based on an empirical algorithm using passive microwave satellite observations from the AMSR-2 (Advanced Microwave Scanning Radiometer 2) sensors on the JAXA satellite GCOM-W1, gridded on a polar stereographic grid (EPSG code 3411, Arctic) with 25...

Major element geochemistry of pyroxenes in metavolcanic rocks of IODP Exp366 samples

Elmar Albers, Wolfgang Bach, Frieder Klein, C D Menzies, Friedrich Lucassen & Damon A H Teagle

Major and trace element geochemistry of carbonates from IODP Exp366

Elmar Albers, Wolfgang Bach, Frieder Klein, C D Menzies, Friedrich Lucassen & Damon A H Teagle

(Table 2) Representative carbonate geochemistry of IODP Exp366 samples

Elmar Albers, Wolfgang Bach, Frieder Klein, C D Menzies, Friedrich Lucassen & Damon A H Teagle
Abbreviations: Arg, aragonite; Cal, calcite.

(Supplementary Tabel 3) Calcium/Iron ratios and adjusted depth of IODP Hole 342-U1410C

Maximilian Vahlenkamp, Igor Niezgodzki, David De Vleeschouwer, Torsten Bickert, Dustin T Harper, Sandra Kirtland Turner, Gerrit Lohmann, Philip F Sexton, James C Zachos & Heiko Pälike

(Table S2) Pore water Sr concentrations and isotopic compositions of IODP Exp366 samples

Elmar Albers, Wolfgang Bach, Frieder Klein, C D Menzies, Friedrich Lucassen & Damon A H Teagle
Given depths are tops of individual cores.WSTP is water-sampling temperature probe; the sample was collected 9.5 days after circulation of drilling fluids had ceased in the bore hole; see Fryer et al. (2018d).

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