Paper No. 6
Presentation Time: 2:40 PM


BAKER, Jonathan L.1, LACHNIET, Matthew S.2, ASMEROM, Yemane3 and POLYAK, Victor J.3, (1)Department of Geoscience, University of Nevada Las Vegas, Box 454010, Las Vegas, NV 89154-4010, (2)Department of Geoscience, University of Nevada Las Vegas, 4505 S. Maryland Parkway, Box 454010, Las Vegas, NV 89154-4010, (3)Earth and Planetary Sciences, University of New Mexico, 221 Yale Blvd, Northrop Hall, Albuquerque, NM 87131,

The past and future impact of climate change on the Volga Basin is a current focus of intensive research by paleoclimatologists and climate modelers. While Holocene climatic shifts are well documented in coastal areas of western Eurasia, however, the past coupling of ocean dynamics and continental climate remains poorly understood, due to the lack of precisely dated, terrestrial climate records. Multi-proxy reconstructions of past hydrological conditions from precisely dated speleothems offer a powerful tool in exploring the impact of Holocene climate dynamics on moisture delivery to the continental interior. We report C- and O-isotope data at 0.5-mm resolution from a 35-cm stalagmite that was collected in growth position from Kinderlinskaya Cave, located in the western foothills of the southern Ural Mountains (56.1°N 55.8°E). The stalagmite, which is the first reported from Russia, grew between 11.8–1.8 ka, according to an age model constructed from 18 U-series dates. Cave monitoring to date confirms the suitability of our sample site (1.8 km from the cave entrance) for paleoclimate reconstruction. Microclimate of the “Brook Room” (RH = 100%; T = 6.2°C) does not vary seasonally, with the exception of a small (0.1°C) but measurable depression in temperature, which corresponds to melting of winter snowpack after a 1-month lag time. These data constrain the timing of speleothem growth and, along with δ18O analysis of cave drip water and local springs, suggest that stalagmite-δ18Ο variability is related to shifts in the δ18O of winter precipitation. Stalagmite δ18O increases along the growth axis from -14.5 to -11 (‰ V-PDB), broadly consistent with early to mid-Holocene warming trends. However, the difference in d18O between Kinderlinskaya Cave and Central European records is anomalously high during the early Holocene and decreases toward ~7 ka. On the other hand, millennial trends closely mimic those recently reported from Sofular Cave (Turkey) for the entire Holocene. Minimum δ13C values at Kinderlinskaya Cave also broadly coincide with humid intervals recorded in Sofular Cave during the Boreal and Atlantic stages. These correlations and discrepancies are explained through shifts in dominant atmospheric circulation modes related to ice-sheet dynamics, solar insolation, and land-sea temperature gradients.