Oxygen isotopes (δ 18O) are the most commonly utilized speleothem proxy and have
provided many foundational records of paleoclimate. Thus, understanding processes …

Reconstructing hydroclimate over the Common Era is essential for understanding the
dominant mechanisms of precipitation change and improving climate model projections …

Tropical hydroclimate in monsoonal regions has been largely understood according to the
orbital monsoon hypothesis, in which rainfall exhibits strong covariation with local summer …

A speleothem collected from Palco Cave (Puerto Rico) spans the 8.2 ka event, a time
interval associated with fluctuations of Atlantic Ocean circulation and possible drying in the …

The 8.2 ka event is the most significant global climate anomaly of the Holocene epoch, but a
lack of records from Mainland Southeast Asia (MSEA) currently limits our understanding of …

ABSTRACT Lake Petén Itzá preserves a sedimentary record spanning the last 413 ka BP,
offering insights into past climate and environmental changes of lowland Central America …