Ostracodes in Owens Lake core OL-92: Alteration of saline and freshwater forms through time

Author(s):  
Claire Carter
Keyword(s):  
2018 ◽  
Vol 90 (2) ◽  
pp. 276-302 ◽  
Author(s):  
Steven N. Bacon ◽  
Nicholas Lancaster ◽  
Scott Stine ◽  
Edward J. Rhodes ◽  
Grace A. McCarley Holder

AbstractReconstruction of lake-level fluctuations from landform and outcrop evidence typically involves characterizing periods with relative high stands. We developed a new approach to provide water-level estimates in the absence of shoreline evidence for Owens Lake in eastern California by integrating landform, outcrop, and existing lake-core data with wind-wave and sediment entrainment modeling of lake-core sedimentology. We also refined the late Holocene lake-level history of Owens Lake by dating four previously undated shoreline features above the water level (1096.4 m) in AD 1872. The new ages coincide with wetter and cooler climate during the Neopluvial (~3.6 ka), Medieval Pluvial (~0.8 ka), and Little Ice Age (~0.35 ka). Dates from stumps below 1096 m also indicate two periods of low stands at ~0.89 and 0.67 ka during the Medieval Climatic Anomaly. The timing of modeled water levels associated with 22 mud and sand units in lake cores agree well with shoreline records of Owens Lake and nearby Mono Lake, as well as with proxy evidence for relatively wet and dry periods from tree-ring and glacial records within the watershed. Our integrated analysis provides a continuous 4000-yr lake-level record showing the timing, duration, and magnitude of hydroclimate variability along the south-central Sierra Nevada.


1994 ◽  
Vol 28 (9) ◽  
pp. 1699-1706 ◽  
Author(s):  
Jeffrey S. Reid ◽  
Robert G. Flocchini ◽  
Thomas A. Cahill ◽  
Robert S. Ruth ◽  
Daniel P. Salgado
Keyword(s):  

2006 ◽  
Vol 56 (11) ◽  
pp. 2623-2629 ◽  
Author(s):  
Elena V. Pikuta ◽  
Takashi Itoh ◽  
Paul Krader ◽  
Jane Tang ◽  
William B. Whitman ◽  
...  

A novel, alkaliphilic, obligately anaerobic bacterium, strain SCAT, was isolated from mud sediments of a soda lake in California, USA. The rod-shaped cells were motile, Gram-positive, formed spores and were 0.4–0.5×2.5–5.0 μm in size. Growth occurred within the pH range 6.7–10.0 and was optimal at pH 8.5. The temperature range for growth was 10–45 °C, with optimal growth at 35 °C. NaCl was required for growth. Growth occurred at 0.5–9.0 % (w/v) NaCl and was optimal at 1–2 % (w/v). The novel isolate was a catalase-negative chemo-organoheterotroph that fermented sugars, proteolysis products, some organic and amino acids, glycerol, d-cellobiose and cellulose. It was also capable of growth by the Stickland reaction. Strain SCAT was sensitive to tetracycline, chloramphenicol, rifampicin and gentamicin, but it was resistant to ampicillin and kanamycin. The G+C content of the genomic DNA was 34.2 mol%. Major fatty acid components were C14 : 0, iso-C15 : 0, C16 : 1 ω9c and C16 : 0. 16S rRNA gene sequence analysis of strain SCAT showed a similarity of approximately 97 % with the type strains of Clostridium formicaceticum and Clostridium aceticum in clostridial cluster XI and a similarity of less than 94.2 % to any other recognized Clostridium species and those of related genera in this cluster. Strain SCAT was clearly differentiated from C. formicaceticum and C. aceticum based on comparison of their phenotypic properties and fatty acid profiles, as well as low levels of DNA–DNA relatedness between strain SCAT and the type strains of these two species. Therefore, strain SCAT is considered to represent a novel species of a new genus, Anaerovirgula multivorans gen. nov., sp. nov., in clostridial cluster XI. The type strain is SCAT (=ATCC BAA-1084T=JCM 12857T=DSM 17722T=CIP 107910T).


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