Peruvian Speleothem Record of Climate and Hydrologic Variability from 167,000 yrs B.P. to 135,000 yrs B.P.

• Main Author: Plummer, Ian
• Format: Text
• Language: unknown
• Published: Union | Digital Works 2022
• Subjects: paleoclimate; peru; speleothem; hydrology; monsoon; MIS 6; caves; hydroclimate; andes; tropics; Geology; Glaciology; Other Earth Sciences; Ice Sheet
• Online Access: https://digitalworks.union.edu/theses/2587; https://digitalworks.union.edu/cgi/viewcontent.cgi?article=3634&context=theses

Peruvian speleothems have been shown to be excellent recorders of paleoclimate by tracking changes in rainfall amount through oxygen isotopes in calcite. Measured changes in rainfall amount have been attributed to changes in the intensity of the South American Seasonal Monsoon (SASM). High insolation in the Southern Hemisphere and low insolation in the Northern Hemisphere is believed to increase the meridional SST gradient, leading to a southerly migration of the mean position of the Inter-Tropical Convergence Zone (ITCZ) and strengthening of the SASM intensity. Conversely, a decrease in Southern Hemisphere insolation and an increase in Northern Hemisphere insolation is believed to have led the ITCZ to a more northerly mean position and weakening of SASM intensity. I present a record from speleothem 19-11, which grew in Pacupahuain Cave between 167,068 yrs B.P. and 135,165 yrs B.P., also known as the penultimate glacial period or Marine Isotope Stage 6 (MIS 6). The δ18O record from 19-11 shows exceptional agreement with overlapping speleothem records from nearby Huagapo Cave (HC). All of these records are anti-phased with 11°S January insolation, supporting the idea that shifts in the mean position of the ITCZ modulate SASM intensity. From 165 ka to 150 ka an increase in δ18O occurs contemporaneously with a decrease in 11°S Jan insolation. This period of time reflects a broad decrease in SASM intensity, a hypothesis corroborated by decreased sediment input into regional lake records. δ18O values are lower at the beginning and end of the 19-11 record, coinciding with 11°S Jan insolation highs. Within long-term insolation driven changes in δ18O, the 19-11 record has rapid oscillations that are also seen in the HC records. Previous researchers have attributed these rapid fluctuations to high-latitude Northern Hemisphere forcing. Increased temperature in the Northern Atlantic and ice sheet melt coincides with apparent weakening of the SASM. This relationship is explained by a weakening of SST gradient and northern ...