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- W156925905 abstract "We present a unique collection of annually banded fossil Montastraea coral colonies from Bonaire (Netherlands Antilles) in the southern Caribbean Sea that reveals growth between ∼AD 800-1050. Coincidentally, this time interval was known for the demise of the classic Maya civilization in the lowlands of the Yucatan Peninsula termed the Terminal Classic Period (roughly AD 750-1050). Explanations for the downfall ranged from foreign invasion to social turmoil, but paleoclimatic evidence suggests severe climate change such as prolonged dry cycles as the primary influence. The Bonaire corals provide the first sub-seasonally resolved proxy records of surface ocean conditions in the Caribbean region during the Terminal Classic Period, and are completely different than the terrestrial-driven and summer-influenced precipitation proxy records from locations in the Yucatan and the Cariaco Basin." @default.
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- W156925905 date "2012-04-01" @default.
- W156925905 modified "2023-09-23" @default.
- W156925905 title "Sub-seasonally resolved coral records of Caribbean sea surface conditions during the demise of the Maya civilization (~ AD 800-1050)" @default.
- W156925905 hasPublicationYear "2012" @default.
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