21,918 Works

Continuous meteorological observations at Georg-von-Neumayer station (1983-06)

Gert König-Langlo
Geocode DATE/TIME has centered values.

Tree-ring width of Abies alba (Miller) from historical object sample HOF12643-301

Jutta Hofmann
Species ABAL; No of rings 73; Begin 1683; End 1755

Tree-ring width of Abies alba (Miller) from historical object sample HOF10539-2

Jutta Hofmann
Species ABAL; No of rings 79; Begin 1462; End 1540

Tree-ring width of Abies alba (Miller) from historical object sample HOF11275-12

Jutta Hofmann
Species ABAL; No of rings 66; Begin 1484; End 1549

Tree-ring width of Abies alba (Miller) from historical object sample HOF11455-6

Jutta Hofmann
Species ABAL; No of rings 74; Begin 1406; End 1479

Mesozooplankton adundance during Mikhail Lomonosov cruise ML14, Part III

Sergey Piontkovski & Alexandra A Shmeleva
Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh size of 0.125 mm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300, 300-500, 500-1000 m) and closed at the upper depth level. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved...

ECHOG_A16_LIG: Control Run for the Last Interglacial (Eemian, 125 kyrBP, DEKLIM-EEM project),monthly mean values

Frank Kaspar & Ulrich Cubasch
Project: Climate change at the end of a warm stage DEKLIM-EEM is a joint project consisting out of 9 individual proposals. The project was financially supported by the German Ministry for Education and Research(BMBF) within the framework of the research programme DEKLIM (www.deklim.de). The purpose of the joint project is to reconstruct the climate of past interglacials and to contribute to the understanding of mechanism that are responsible for the transition to a cold stage....

Expanded measurements from Neumayer Station (1998-04)

Gert König-Langlo
99999: No clouds detected

(Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-853B

David McGee, Franco Marcantonio & Jean Lynch-Stieglitz

(Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-852A

David McGee, Franco Marcantonio & Jean Lynch-Stieglitz

(Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-851E

David McGee, Franco Marcantonio & Jean Lynch-Stieglitz

(Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-849A

David McGee, Franco Marcantonio & Jean Lynch-Stieglitz

(Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-848B

David McGee, Franco Marcantonio & Jean Lynch-Stieglitz

(Table 2) Oxygen and thorium isotope ratios, and flux data of ODP Hole 138-850A

David McGee, Franco Marcantonio & Jean Lynch-Stieglitz

Tree-ring width of Abies alba (Miller) from historical object sample HOF10782-8

Jutta Hofmann
Species ABAL; No of rings 59; Begin 1689; End 1747

Oxygen isotopes, trace elements and age for coral core Gua 1, slab A

Steffen Hetzinger
Ordinal number is equal to new no. in reference

Concentrations of chlorophyll-alpha in water of the Aegean Sea at Station SEPT-1998-IR39

Kalliopi Pagou & Georgia Assimakopoulou
Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).

Microplankton abundance at Station MARCH-1997-GN36199704601MSB06 in the euphotic zone of the Aegean Sea in spring 1997. Part 2 - dinoflagellates

Olympia Gotsis-Skretas, Kalliopi Pagou, Lydia Ignatiades & Stella Psarra
Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger phytoplankton cells (>5µm) were preserved in alkaline Lugol solution. Utermoehl, H., 1958. Zur Vervollkommung der quantitativen Phytoplankton-Methodik. Mitt. Int. Ver. Theor. Angew. Limnol., 9:1-38.

Physical oceanography at CTD station JUNE-1998-IR18

Dimitrios Georgopoulos & Vassilis Zervakis

Registration Year

  • 2008
    21,918

Resource Types

  • Dataset
    21,918

Data Centers

  • PANGAEA
    21,891
  • Geoforschungszentrum Potsdam
    24
  • World Data Center for Climate
    3