Publications Published in Quaternary Science Reviews

1. Abrupt climate change around 22 ka on the Siple Coast of Antarctica. Taylor, K C; White, J W C; Severinghaus, J. P.; Brook, E J; Mayweski, P A; Alley, R B; Steig, E J; Spencer, M K; Meyerson, E; Meese, D A; Lamorey, G W; Grachev, A; Gow, A J; Barnett, B A.
   Quaternary Science Reviews: 2004
   Notes
   A new ice core from Siple Dome, Antarctica suggests the surface temperature increased by B6 C in just several decades at approximately 22 ka BP. This abrupt change did not occur 500km away in the Byrd ice core, or in climate proxy records in the Siple Dome core indicative of the mid-latitude Pacific. This demonstrates there was significant spatial heterogeneity in the response of the Antarctic climate during the last deglaciation and draws attention to unexplained mechanisms of abrupt climate change in Antarctica.
   
   
   
2. Holocene multidecadal and multicentennial droughts affecting Northern California and Nevada. Benson, L.; Kashgarian, M.; Rye, R.; Lund, S.; Paillet, F.; Smoot, J.; Kester, C.; Mensing, S.; Meko, D.; Lindstrom, S..
   Quaternary Science Reviews: 2002
   Notes
   Continuous, high-resolution delta(18)O records from cored sediments of Pyramid Lake, Nevada, indicate that oscillations in the hydrologic balance occurred, on average, about every 150 years (yr) during the past 7630 calendar years (cal yr). The records are not stationary; during the past 2740 yr, drought durations ranged from 20 to 100 yr and intervals between droughts ranged from 80 to 230 yr. Comparison of tree-ring-based reconstructions of climate change for the past 1200 yr from the Sierra Nevada and the El Malpais region of northwest New Mexico indicates that severe droughts associated with Anasazi withdrawal from Chaco Canyon at 820 cal yr BP (calendar years before present) and final abandonment of Chaco Canyon, Mesa Verde, and the Kayenta area at 650 cal yr BP may have impacted much of the western United States. During the middle Holocene (informally defined in this paper as extending from 8000 to 3000 cal yr BP), magnetic susceptibility values of sediments deposited in Pyramid Lake's deep basin were much larger than late-Holocene (3000-0 cal yr BP) values, indicating the presence of a shallow take. In addition, the mean delta(18)O value of CaCO3 precipitated between 6500 and 3430 cal yr BP was 1.6parts per thousand less than the mean value of CaCO3 precipitated after 2740 cal yr BP. Numerical calculations indicate that the shift in the delta(18)O baseline probably resulted from a transition to a wetter ( > 30%) and cooler (3-5degreesC) climate. The existence of a relatively dry and warm middle-Holocene climate in the Truckee River-Pyramid Lake system is generally consistent with archeological, sedimentological, chemical, physical, and biological records from various sites within the Great Basin of the western United States. Two high-resolution Holocene-climate records are now available from the Pyramid and Owens lake basins which suggest that the Holocene was characterized by five climatic intervals. TIC and 6180 records from Owens Lake indicate that the first interval in the early Holocene (11,600 10,000 cal yr BP) was characterized by a drying trend that was interrupted by a brief (200 yr) wet oscillation centered at 10,300 cal yr BP. This was followed by a second early-Holocene interval (10,000-8000 cal yr BP) during which relatively wet conditions prevailed. During the early part of the middle Holocene (8000-6500 cal yr BP), high-amplitude oscillations in TIC in Owens Lake and delta(18)O in Pyramid Lake indicate the presence of shallow lakes in bomb basins. During the latter part of the middle Holocene (6500 3800 cal yr BP), drought conditions dominated, Owens Lake desiccated, and Lake Tahoe ceased spilling to the Truckee River, causing Pyramid Lake to decline. At the beginning of the late Holocene (similar to 3000 cal yr BP), Lake Tahoe rose to its sill level and Pyramid Lake increased in volume. (C) 2002 Elsevier Science Ltd. All rights reserved.