scholarly journals Revised chronology for late Pleistocene Mono Lake sediments based on paleointensity correlation to the global reference curve

2006 ◽  
Vol 252 (1-2) ◽  
pp. 94-106 ◽  
Author(s):  
Susan H. Zimmerman ◽  
Sidney R. Hemming ◽  
Dennis V. Kent ◽  
Stephanie Y. Searle
Keyword(s):  
Lake Sediments ◽  
Late Pleistocene ◽  
Mono Lake ◽  
Reference Curve

SOURCES OF CARBONATE PRECIPITATION IN MONO LAKE SEDIMENTS: δ18O AND CARBONATE CLUMPED ISOTOPES AS LAKE LEVEL PROXIES

2017 ◽  
Author(s):  
Miquela Ingalls ◽  
◽  
Sophie Westacott ◽  
Makayla Betts ◽  
Jana Meixnerova ◽  
...  
Keyword(s):  
Lake Sediments ◽  
Lake Level ◽  
Mono Lake ◽  
Carbonate Precipitation ◽  
Clumped Isotopes

scholarly journals Separation and 14C Dating of Pure Pollen from Lake Sediments: Nanofossil AMS Dating

Radiocarbon ◽  
1992 ◽  
Vol 34 (3) ◽  
pp. 557-560 ◽  
Author(s):  
Austin Long ◽  
Owen K. Davis ◽  
Jeanne de Lanois
Keyword(s):  
Organic Matter ◽  
Lake Sediments ◽  
Mono Lake ◽  
Bulk Sediment ◽  
Clean Room ◽  
14C Dating ◽  
Ams Dating

We have developed and tested a practical device for manually separating pollen from pollen concentrates in sufficient quantity for AMS 14C dating. It is a combination of standard, commercially available equipment handled in a clean room by an individual trained to recognize pollen. A typical example requires about 15–20 h of hand-picking under the microscope. We show the usefulness of this procedure with results on a mid-Holocene segment from a core from Mono Lake. Sediments from this hardwater lake contain pollen and finely disseminated organic matter, but no macrofossils. The pollen dated ca. 1000 yr younger than the bulk sediment. The sediment “date” is most likely affected by incorporation of limestone-derived carbon, and is erroneously old.

scholarly journals Stable isotope studies on Mono Lake (California). 1. d18 in lake sediments as proxy for climatic change during the last 150 years

1997 ◽  
Vol 42 (2) ◽  
pp. 230-238 ◽  
Author(s):  
Hong-Chun Li ◽  
Teh-Lung Ku ◽  
Lowell D. Stott ◽  
Robert F. Anderson
Keyword(s):  
Stable Isotope ◽  
Lake Sediments ◽  
Climatic Change ◽  
Mono Lake ◽  
Isotope Studies

scholarly journals Supplemental Material: Thermodynamic evaporation and freshwater mixing models to test salinity proxies for late Pleistocene lake levels, Mono Lake, California

2021 ◽  
Author(s):  
Rahul Sahajpal
Keyword(s):  
Late Pleistocene ◽  
Computer Code ◽  
Mono Lake ◽  
Geochemical Evolution ◽  
Mixing Models ◽  
Glacial Period ◽  
Lake Levels ◽  
Last Glacial Period ◽  
Lake Waters ◽  
The Last Glacial

A Python-based computer code used for automating the simulation used to predict the geochemical evolution of Mono Lake waters since the last glacial period.<br>

RADIOCARBON DATING POLLEN GRAINS SORTED BY FLOW CYTOMETRY FROM LAKE SEDIMENTS OF MONO LAKE (CALIFORNIA)

2017 ◽  
Author(s):  
Irene Tunno ◽  
◽  
Susan H. Zimmerman ◽  
Tom Brown ◽  
Christiane A. Hassel
Keyword(s):  
Flow Cytometry ◽  
Lake Sediments ◽  
Radiocarbon Dating ◽  
Pollen Grains ◽  
Mono Lake

Lake sediments from Store Koldewey, Northeast Greenland, as archive of Late Pleistocene and Holocene climatic and environmental changes

Boreas ◽  
2009 ◽  
Vol 38 (1) ◽  
pp. 59-71 ◽  
Author(s):  
MARTIN KLUG ◽  
STEFFI SCHMIDT ◽  
OLE BENNIKE ◽  
OLIVER HEIRI ◽  
MARTIN MELLES ◽  
...  
Keyword(s):  
Lake Sediments ◽  
Late Pleistocene ◽  
Environmental Changes

Late Pleistocene glaciers in Darhad Basin, northern Mongolia

2008 ◽  
Vol 69 (2) ◽  
pp. 169-187 ◽  
Author(s):  
Alan R. Gillespie ◽  
Raymond M. Burke ◽  
Goro Komatsu ◽  
Amgalan Bayasgalan
Keyword(s):  
Central Asia ◽  
Lake Sediments ◽  
Late Pleistocene ◽  
Cosmic Ray ◽  
Luminescence Dating ◽  
Equilibrium Line ◽  
Equilibrium Line Altitude ◽  
Exposure Dating ◽  
Northern Mongolia ◽  
Dammed Lake

Late Pleistocene glaciers around Darhad Basin advanced to near their maximum positions at least three times, twice during the Zyrianka glaciation (at ∼ 17–19 ka and ∼ 35–53 ka), and at least once earlier. The Zyrianka glaciers were smaller than their predecessors, but the equilibrium-line altitude (ELA) difference was < 75 m. End moraines of the Zyrianka glaciers were ∼ 1600 m asl; ELAs were 2100–2400 m asl.14C and luminescence dating of lake sediments confirm the existence of paleolake highstands in Darhad Basin before ∼ 35 ka. Geologic evidence and10Be cosmic-ray exposure dating of drift suggests that at ∼ 17–19 ka the basin was filled at least briefly by a glacier-dammed lake ∼ 140 m deep. However, lake sediments from that time have not yet been recognized in the region. A shallower paleolake briefly occupied the basin at ∼ 11 ka, but between ∼ 11 and 17 ka and after ∼ 10 ka the basin was probably largely dry. The timing of maximum glacier advances in Darhad appears to be approximately synchronous across northern Mongolia, but different from Siberia and western Central Asia, supporting the inference that paleoclimate in Central Asia differed among regions.

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