To integrate the information retrieved from regionally to globally distributed palaeoceanographic and palaeoclimatic records. |
A1 A2 A4 A5
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B2 B3
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C1 C3 C7
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D3
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To exploit the continuous nature of the oceanic sedimentary record to reconstruct the history of Earth's climate. |
A1 A2 A4 A5
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B2 B3
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C1 C3 C7
|
D3
|