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The tracks, they added, were found only in association with deposits indicating damp to dry conditions.
This complements the results from DRIFTS analysis of the deposits indicating polyaromatic hydrocarbons.
More than 50% of the succession consists of mass-transport deposits, indicating significant slope instability.
This peak supports the results obtained from the DRIFTS analysis of the deposits indicating the presence of oxygenated groups such as carboxylic acids, anhydrides or lactones on the deposits [13 15].
c) Human influence on the landscape is reflected in colluvial and alluvial deposits indicating the occurrence of human-induced soil erosion and is dated prior to the beginning of the Bronze Age (here corresponding to Subboreal period).
Important terrestrial and aquatic vertebrate fossils are primarily preserved within fluvial and fluvio-lacustrine deposits, indicating that the terrestrial Karungu fauna lived in a relatively dry and open habitat.
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These deposits indicate a depositional environment of rivers draining into freshwater lakes in a generally arid or semiarid region, which from paleomagnetic evidence appears to have been located about 20° north of the paleoequator.
Optically stimulated luminescence (OSL) dating of sandy beds within coarse-grained alluvial deposits indicates that deposition of alluvium shed from the Pine Mountain massif occurred near the southern margin of the Cuyama structural basin at the elevation of the Cuyama River between 25 and 14 ka.
New 40Ar/39Ar ages of volcanic ashes intercalated with the lake deposits and the overlying fluvial deposits indicate that lacustrine diatomite-rich deposition had begun by 10.86 ± 0.04 Ma, and the final stage of incision of a canyon through the lake deposits is younger than 3.04 ± 0.03 Ma.
Atomic force microscopy characterization of the deposits indicated that electrochemical parameters and the deposition method (galvanostatic or potentiostatic) influence the morphology of the deposits.
Optically Stimulated Luminescence (OSL) dating of these deposits indicates formation between 44 and 20 ka, with the possibility that deposition occurred during two phases of rapid sedimentation at ca. 42 and 25 ka.
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