Directly dated MIS 3 Lake-Level Record from Lake Manix, Mojave Desert, California, USA

• Published in: Quaternary Research
• Main Authors: Reheis, Marith C., Miller, David M., McGeehin, John P., Redwine, Joanna R., Oviatt, Charles G., Bright, Jordon
• Other Authors: U.S. Geological Survey (USGS) Climate and Land Use Research and Development Program
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2015
• Subjects: Pacific; North Atlantic
• Online Access: http://dx.doi.org/10.1016/j.yqres.2014.11.003; http://api.elsevier.com/content/article/PII:S0033589414001318?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:S0033589414001318?httpAccept=text/plain; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400028027

Abstract An outcrop-based lake-level curve, constrained by ~ 70 calibrated 14 C ages on Anodonta shells, indicates at least 8 highstands between 45 and 25 cal ka BP within 10 m of the 543-m upper threshold of Lake Manix in the Mojave Desert of southern California. Correlations of Manix highstands with ice, marine, and speleothem records suggest that at least the youngest three highstands coincide with Dansgaard–Oeschger (D–O) stadials and Heinrich events 3 and 4. The lake-level record is consistent with results from speleothem studies in the Southwest that indicate cool wet conditions during D–O stadials. Notably, highstands between 43 and 25 ka apparently occurred at times of generally low levels of pluvial lakes farther north as interpreted from core-based proxies. Mojave lakes may have been supported by tropical moisture sources during oxygen-isotope stage 3, perhaps controlled by southerly deflection of Pacific storm tracks due to weakening of the sea-surface temperature gradient in response to North Atlantic climate perturbations.