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Presently, the core site is situated beneath a seasonally varying low-salinity tongue which is advected from the Java Sea via the Sunda Strait. It carries terrigenous matter of a characteristic signature. During the last glacial period stage , when sea level was lower than during the Holocene, the Sunda Strait was closed and the terrigenous supply from that source ceased.
As the core site is close to the equator, our results indicate that atmospheric and oceanographic circulation was alternatively dominated by the Northern Hemisphere East Asian Monsoon system and the Southern Hemisphere Australian Monsoon system. Increased mixing of the surface waters led to a slight rise in paleoproductivity. A similar but much weaker situation prevailed from 74 to 70 ka.
During most of the glacial period, from 70 to 20 ka, strong northeasterly winds associated with the East Asian Winter Monsoon intensified the Indian Monsoon Current and the eastward flowing SJC, and may have also carried dust across the equator to our core site. During this glacial phase, populations of the giant diatom Ethmodiscus rex were thriving and may indicate a reduced deep and intermediate thermohaline circulation at the site. The monsoonal system as we know it today, with distinct dry and wet seasons, may not have been active before V12 ka.
All rights reserved. Keywords: South Java Current; clay minerals; monsoon; paleoceanography; glacial; Holocene; Ethmodiscus rex 1. E-mail address: [email protected] F. Gingele et al. However, with Phytoplankton productivity in this part of the eastern Indian Ocean is low, except for an area south of Java, where weak seasonal upwelling brings nutrients to the sea surface Wyrtki, ; Martinez et al. However, the present oceanographic and climatic system may have been established rather recently and been active for only 10 ka De Deckker et al.
Sea level was substantially lower, not only during the last glacial maximum LGM , but for most of the past 80 ka Chappell et al. Results from marine as well as continental climate records indicate that precipitation in the Indonesian Archipelago van der Kaars, , ; van der Kaars and Dam, ; De Deckker et al.
Synchronism of paleoclimatic events in the Northern and Southern Hemisphere has been discussed extensively on the basis of various continental and marine paleoclimate proxies.
An, In our investigation area, there is evidence from modern meteorological data and paleoclimate records that the East Asian Monsoon and the Australian Monsoon system are linked by transequatorial air streams An, Deep-sea core BAR is located close to the equator below the path of the present SJC and provides a continuous record of the past 80 ka.
Biogenic and terrigenic proxies are used to decipher changes in current directions and properties of the involved water masses and construct a conclusive paleoceanographic and paleoclimatic scenario. The core consists of 9. This zone was probably disturbed during the coring procedure. The piston core and the associated trigger core were sampled at cm intervals. Lithology, carbon- and oxygen-isotope records Globigerinoides ruber of core BAR Short solid lines are carbon- and oxygen-isotope records of the trigger core.
For comparison planktonic and benthonic oxygenisotope records from core from the South China Sea, which have a similar resolution Wang et al. Isotope stages and position of the Toba ash in this core after Bu«hring and Sarnthein Contents of each clay mineral group in the sample are expressed as relative percentage.
Carbonate was measured on dry bulk samples using a standard titration method. NaOH with a concentration of 0. The abundance of the giant diatom Ethmodiscus rex in the fraction s 63 Wm, which can be rather expressed by the volume of the fraction than by the weight, was assessed by roughly estimating the volume of the fraction s 63 Wm in a glass vial, subdivided by six evenly spaced arbitrary markings.
Stratigraphy and age control The age model of core BAR is based on the cm spaced N18 O record of the planktonic foraminifera Globigerinoides ruber. Individual isotope events 2. The ages for 2. A distinct ash layer with a sharp base was found in the core at 8. Chemical analysis of glass shards and pumice was performed by microprobe and gave ambiguous results. Therefore the ash layer was not used as a stratigraphic marker.
The base of the core terminates at Comparison of the N18 O record of the piston core BAR to the N18 O values from the uppermost 70 cm of the trigger core, which is supposed to contain the sediment surface somewhat undis- turbed, shows a lag between both records. The clay mineral data from the trigger core show a similar lag.
A core from the South China Sea recently published by Wang et al. Apart from a few freshwater spikes in the planktonic record, a striking similarity to BAR is obvious Fig. Biogenic proxies Biogenic components in marine sediments can provide proxy-data on paleoproductivity and nutrients, ocean chemistry and circulation, sea-surface temperatures and salinity for a comprehensive summary see Fischer and Wefer, Oxygen- and carbon-isotope records Globigerinoides ruber , linear sedimentation rate, bulk carbonate and abundance of Ethmodiscus rex in core BAR against age.
The N13 C record of Globigerinoides ruber shows a typical pattern of low glacial and high Holocene values.
The maximum amplitude between the glacial and the Holocene values is 1x, but on average the shift between the Holocene and the glacial period between 40 and 20 ka is only 0. Antarctic Intermediate Water Mulitza et al. Udit sings for Shahrukh. Holi Special. Hum Aapke Hain Koun.
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