407,345 Works

Uncalibrated radiocarbon ages, IODP Expedition 325

Light reflectance (RGB) of Hole 325-M0058A

Moisture and density (MAD) measured on IODP Hole 325-M0032A

Moisture and density (MAD) measured on IODP Hole 325-M0057A

Moisture and density (MAD) measured on IODP Hole 325-M0058A

Light reflectance (RGB) of Hole 325-M0043A

Light reflectance (RGB) of Hole 325-M0049B

Moisture and density (MAD) measured on IODP Hole 325-M0039A

(Table 1) Mineral composition of samples from the Lost Village hydrothermal field

O M Dara, Tatyana G Kuz'mina & Alla Yu Lein

Community structure and biodiversity in marine benthic communities during experiments, 2011, supplement to: Hale, Rachel; Calosi, Piero; McNeill, Lisa; Mieszkowska, N; Widdicombe, Stephen (2011): Predicted levels of future ocean acidification and temperature rise could alter community structure and biodiversity in marine benthic communities. Oikos, 120(5), 661-674

Rachel Hale, Piero Calosi, Lisa McNeill, N Mieszkowska & Stephen Widdicombe
A mesocosm experiment was conducted to quantify the effects of reduced pH and elevated temperature on an intact marine invertebrate community. Standardised faunal communities, collected from the extreme low intertidal zone using artificial substrate units, were exposed to one of eight nominal treatments (four pH levels: 8.0, 7.7, 7.3 and 6.7, crossed with two temperature levels: 12 and 16°C). After 60 days exposure communities showed significant changes in structure and lower diversity in response to...

(Table 1) Carbonate mineralogical and isotopic analyses of carbonate subsamples from station TV-GKG 40

Jens Greinert, Gerhard Bohrmann & Marcus Elvert

(Table 2) Isotopic analyses from TVG 97

Jens Greinert, Gerhard Bohrmann & Marcus Elvert
Crust samples are Mg-calcite with 7 mol% MgCO3. Acharax samples are pure calcite.

Moisture and density (MAD) measured on IODP Hole 325-M0042A

Moisture and density (MAD) measured on IODP Hole 325-M0043A

Moisture and density (MAD) measured on IODP Hole 325-M0049A

Moisture and density (MAD) measured on IODP Hole 325-M0052A

Light reflectance (RGB) of Hole 325-M0037A

Light reflectance (RGB) of Hole 325-M0040A

Geochemistry on interstitial water collected from transect NOG-01B, IODP Expedition 325

QAQC documentation is available at 'Further details', for raw data and standards measurements see 'Other version'.

(Table 1) Location of stations within the Malama Bay with respect to the diffuser, biomasses of heterotrophic bacteria and their percentages relative to biomasses at background stations

Vladimir I Vedernikov, V G Bondur, Mikhail E Vinogradov, Michael R Landry & M N Tsidilina

(Table 2) Concentration of chlorophyll a and biomass of different planktonic communities at stations in the area of the diffuser in the Mamala Bay

Vladimir I Vedernikov, V G Bondur, Mikhail E Vinogradov, Michael R Landry & M N Tsidilina

(Table 4) Eutrophication factors in the Mamala Bay calculated from integral biomasses of different planktonic communities and integral content of chlorophyll a

Vladimir I Vedernikov, V G Bondur, Mikhail E Vinogradov, Michael R Landry & M N Tsidilina

Swath sonar bathymetry during POLARSTERN cruise ANT-V/4 (PS10) with links to multibeam raw data files

Hans Werner Schenke & Fred Niederjasper
Multibeam data were collected during R/V Polarstern cruise ANT-V/4. Data recording was executed in southern Weddell Sea off Antarctic ice shelf and was supervised by two hydrographers. Data are unprocessed and may contain outliers and blunders. Therefore the data should not directly be used for grid calculations and charting projects but need to be edited furthermore. One file normally contains a measurement period of one day. The dataset consists of 58 files in originally Seabeam...

Swath sonar bathymetry during POLARSTERN cruise ANT-IV/4 (PS08) with links to multibeam raw data files

Klemens Heidland & Hans Werner Schenke
Multibeam data were collected during R/V Polarstern cruise ANT-IV/4. Data recording was executed on transit from Cape Town to Mandela Fracture Zone, Maud Rise and Punta Arenas and was supervised by one hydrographer. Data are unprocessed and may contain outliers and blunders. Therefore the data should not directly be used for grid calculations and charting projects but need to be edited furthermore. One file normally contains a measurement period of one day. The dataset consists...

(Table 2) Sediment thickness and sedimentation rates for lowstand, transgression and highstand phases of sea level at the Great Barrier Reef Shelf

Gavin B Dunbar, Gerald Roy Dickens & Robert M Carter

Registration Year

  • 2022
    8,086
  • 2021
    8,135
  • 2020
    11,751
  • 2019
    6,479
  • 2018
    9,313
  • 2017
    12,121
  • 2016
    9,373
  • 2015
    12,319
  • 2014
    11,598
  • 2013
    16,063

Resource Types

  • Dataset
    396,695
  • Collection
    10,463

Affiliations

  • University of Iowa
    41
  • University of Duisburg-Essen
    6
  • Bjerknes Centre for Climate Research
    5
  • Alfred Wegener Institute - Wadden Sea Station Sylt
    5
  • Geophysical Institute, University of Bergen
    5
  • MARUM - Center for Marine Environmental Sciences, University Bremen
    5
  • Boston University
    5
  • Leibniz-Zentrum für Marine Tropenforschung, Bremen, Germany
    4
  • Leibniz-Institut für Medienforschung | Hans-Bredow-Institut
    4
  • Institute of Mineralogy, Leibniz University of Hannover
    4