CHANGING PATTERNS IN HOLOCENE PRECIPITATION AS RECORDED BY DOMINICAN CORAL PROXIES
High-resolution oxygen isotopic data from Enriquillo corals reflect a decrease in the seasonal amplitude of Holocene precipitation as governed by changes in orbital induced insolation from ~7.2 ka to ~5.3 ka. A decrease in summer precipitation may be attributed to a decrease in the latitudinal extent of the Atlantic Intertropical Convergence Zone (ITCZ). In addition to a strong seasonal mode of variability, oscillations in the geochemical composition of these corals occur with a consistent frequency of 15-20 years. The decadal to multi-decadal mode of variability appears to represent regional fluctuations in tropical storm-related precipitation. Sustained periods of isotopic depletion are attributed primarily to the multi-year influx of rivers during and after the passage of storms. The cyclic post-storm diversion of rivers occurred as alluvial shedding from the surrounding mountains forced the river toward more northerly drainage paths. A mechanism whereby tropical Atlantic sea surface temperature patterns and/or thermohaline circulation mediate Mid-Holocene tropical storm cyclicity is invoked. Enriquillo corals may also record millennial scale reversals in regional SST and/or precipitation during the Mid-Holocene. The oxygen isotopic compositions of Enriquillo corals are interpreted to indicate the onset and termination of a Mid-Holocene wet/warm period at ~7 ka and 5.9-5.3 ka respectively. These dates are in agreement with other proxy records of a Mid-Holocene moist/humid period from the tropical Atlantic and Africa. These millennial scale events are likely forced by complex changes in ocean/atmosphere dynamics.