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Survey data collected from Core E53-10, located on the edge of the South Tasman rise
Most globally linked climatic records dealing with continuous longterm change are derived from the ocean sea-floors where sedimentation of microplankton is accumulated on a time... -
Raw counts of diatom species in 18 surface samples collected during the...
Diatom distributions in the polar regions have been attributed to physical and biological processes. To contribute to an existing diatom database (Pichon et al. 1992), 18... -
Phytolith recovery from core MD88-779
Core MD88-779 was taken during the 1988 French APSARA IV cruise in the South East Indian Ocean. The core was situated on the South Tasman Rise (47º50.690S, 146º32.750E) at a... -
Historical February / September sea-ice concentration and annual sea-ice...
Variations in microfossil records in sediments over time are used as proxies for changes in the ocean. One important record determined from microfossils is sea-ice cover which... -
Historical February Sea-Surface Temperature Estimates Utilising Diatom...
The purpose of this study was to estimate past sea-surface temperature in the Southeast Indian Ocean. The accumulation of diatom microplankton assemblages in sediments being the... -
Historical February Sea-Surface Temperature Estimates Utilising Diatom...
The purpose of this study was to estimate past sea-surface temperature in the Southeast Indian Ocean. The accumulation of diatom microplankton assemblages in sediments being the... -
Historical August Sea-Surface Temperature Estimates Utilising a Diatom...
The purpose of this study was to estimate past sea-surface temperature in the Southeast Indian Ocean. The accumulation of diatom microplankton assemblages in sediments being the... -
Diatom recovery from core MD88-787: Raw counts
Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Diatom recovery from core MD88-784: Raw counts
Core MD88-784 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Diatom recovery from core MD88-779: Raw counts
Core MD88-779 was taken during the 1988 French ASPARA IV cruise in the South East Indian Ocean aboard the Marion Dufresne. The core is situated on the South Tasman Rise...