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Influences on the fractionation of calcium isotopes in planktonic foraminifera
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Cryogenic bolometric radiometer and telescope
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A large West Antarctic Ice Sheet explains Early Neogene sea-level amplitude
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A Large West Antarctic Ice Sheet Explains Early Neogene Sea-Level Amplitude
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A Large West Antarctic Ice Sheet Explains Early Neogene Sea-Level Amplitude
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A Large West Antarctic Ice Sheet Explains Early Neogene Sea-Level Amplitude
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A Large West Antarctic Ice Sheet Explains Early Neogene Sea-Level Amplitude
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A Large West Antarctic Ice Sheet Explains Early Neogene Sea-level Amplitude
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A Large West Antarctic Ice Sheet Explains Early Neogene Sea-level Amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic ice sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude
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