Brief description
The advent of deep-sea drilling in the 1950's prompted the use of planktonic foraminifera (unicellular protozans) as palaeoceanographic indicators. They provide a natural archive of past environmental changes due to their global distribution, their prolific productivity and sensitivity to environmental variations. The most abundant species within core MD002361 is the subtropical species Gs. ruber. High abundances =30% are seen during the interglacial periods Marine Isotope Stages (MIS) 11, 9, 7, 5 with peak abundance (37.7%) during the Holocene. Other tropical and subtropical species follow this pattern. The transitional, deep dwelling species Gr. inflata has the most distinct abundance change within core MD002361. This species is absent during the interglacial periods but achieves high relative abundances (~20-30%) during glacial periods.Lineage
Maintenance and Update Frequency: notPlannedParameters: Age of core (yrs BP), relative abundance of planktonic foraminifera assemblages (%).
Notes
CreditThe Australian National University (ANU)
Funded by The National Oceans Office (NOO)
Funded by The French Polar Institute
Funded by The Australian Research Council (ARC)
Funded by The Australian Institute of Nuclear Science Engineering (AINSE)
Funded by The Murray Darling Basin Commission
To reconstruct the faunal assemblages of planktonic foraminifera through time and to give insight into the palaeoceanography of the core location.
Issued: 22 03 2007
Data time period: 2000-01-01 to 2000-01-01
text: westlimit=113; southlimit=-22.5; eastlimit=113.5; northlimit=-22
text: uplimit=2034; downlimit=2034
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(ANU_Spooner_MD002361_3_data.xls)
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