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| | SITE 1150 |
 | | Whereas this may not be of significance in terms of long-term shifts, those investigating high-resolution paleoceanographic and paleoclimatic shifts from ODP piston cores should be mindful of this issue, which will only be revealed in the rare instances where marker horizons are present and confirmed as such (see also Robinson, 1990). |
 | | Although these are the only widespread terrestrial and marine tephras that we have suggested may potentially correlate with Site 1150 tephras, there may be further correlative potential with additional tephras in the Japan region, including both Holocene and Pleistocene deposits. |
 | | Finally, for Site 1150, one tephra layer (Sample 186-1150A-9H-3, 2-4 cm) is, in comparison with the dominantly rhyolitic tephras from Sites 1151 and 1150 and the Quaternary terrestrial record, uncharacteristically andesitic to dacitic (Fig. |
| www-odp.tamu.edu /publications/186_SR/107/107_10.htm (558 words) |
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