Oxygen-isotope variations in post-glacial Lake Ontario
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文摘

Lakewater in glacial sediments has low δ18Olakewater (< –17‰).

Meltwater pulse is observed before onset of hydrologic closure.

Ostracodes indicate no inundation of seawater in early Lake Ontario.

Early Holocene Lake Ontario shows progressive increase in δ18Olakewater.

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