Radiolarians from ODP Leg 116 holes

Cores recovered from three sites of Leg 116 were studied for radiolarians. Generally, radiolarians were absent from most samples prepared for examination. Moderate to well-preserved radiolarian assemblages are found only in the uppermost one or two cores that were the focus of this study. All of the radiolarian assemblages in the upper cores belong to the Buccinosphaera invaginata Zone of latest Quaternary age. However, there is one stratum where a few Miocene radiolarians are reworked into the modern assemblages. Local seamounts are suggested sources for the reworked radiolarians

(Table 1) Calcareous nannofossil distribution at ODP Site 180-1109 from the Solomon Sea, western Pacific

The paleoceanography of the Solomon Sea for the last 195,000 years was investigated, based on the observations of 21 taxonomic groups of calcareous nannofossils in 144 samples taken from tocean drilling program (ODP) cores 1109A-1H and 1109C-2H. Oxygen isotope ratios in tests of the planktonic foraminifer Globigerinoides ruber allow us to assign the cores to oxygen isotope stages 7-1. Past sea-surface temperatures (SST) were estimated qualitatively using the composition of three Gephyrocapsa coccolith morphotypes; the high-, intermediate- and low-angel types that are classified based on the bridge angle of coccolith, can be used as proxies for warm, intermediate and cold temperature, respectively. Abundance of the high-angel type coccoliths increased and decreased during the interglacial and glacial periods, respectively. This tendency is consistent with the expected change of the Western Pacific Warm Pool (WPWP) development. However, a large shift in the abundance of the high-angle type coccolith recorded during early stage 3 did not correspond to the oxygen isotope record. The ratio of small (<2.5 µm) placoliths of Reticulofenetsra and Gephyrocapsa to the low-photic species was higher during stage 2 than late stage 3 and 1. As the reduced blanketed effect to the WPWP would cause an increase in the number of small placoliths, a reduction of the WPWP in stage 2 is indicated by the increase of small placoliths and by the lower SST deduced from the composition of the Gephyrocapsa morphotypes. The decreasing trend of small placoliths after ~40 ka is similar to the results reported in several previous studies in the surrounding regions of Australia