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0.9 Ma oxygen isotope stratigraphy for a shallow-water sedimentary transect across three IODP 317 sites in the Canterbury Bight of the southwest Pacific Ocean
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文摘

0.9 Ma δ18O stratigraphy for IODP 317 in the Canterbury Bight is established.

Glacial-interglacial cycles are recognized along a shallow-water sedimentary transect.

Sedimentary features co-vary with the planktonic and benthic δ18O values.

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