Late Pleistocene-Holocene alluvial stratigraphy of southern Baja California, Mexico

QUATERNARY SCIENCE REVIEWS

卷:146

Article

Antinao, Jose Luis^1,2  McDonald, Eric¹  Rhodes, Edward J.³  Brown, Nathan³  Barrera, Wendy³  Gosse, John C.⁴  Zimmermann, Susan⁵ 

[1] Desert Res Inst, Div Earth & Ecosyst Sci, 2215 Raggio Pkwy, Reno, NV 89512 USA

[2] CIGIDEN, Natl Res Ctr Integrated Nat Disaster Management, Santiago 7820436, Chile

[3] Univ Calif Los Angeles, Dept Earth & Space Sci, Los Angeles, CA 90095 USA

[4] Dalhousie Univ, Dalhousie Geochronol Ctr, Halifax, NS B3H 4J1, Canada

[5] Lawrence Livermore Natl Lab, Ctr Accelerator Mass Spectrometry, Livermore, CA 94550 USA

关键词: Late Pleistocene;    Holocene;    Alluvial fans;    Tropical cyclones;    Baja California;    North America;    Sonoran desert;    Mexico;   

DOI  :  10.1016/j.quascirev.2016.06.008

来源: Elsevier

【 摘 要 】

A late Pleistocene to Holocene alluvial stratigraphy has been established for the basins of La Paz and San Jose del Cabo, in the southern tip of the Baja California peninsula, Mexico. Six discrete alluvial units (Qt1 through Qt6) were differentiated across the region using a combination of geomorphologic mapping, sedimentological analysis, and soil development. These criteria were supported using radiocarbon, optically stimulated luminescence and cosmogenic depth-profile geochronology. Major aggradation started shortly after similar to 70 ka (Qt2), and buildup of the main depositional units ended at similar to 10 ka (Qt4). After deposition of Qt4, increasing regional incision of older units and the progressive development of a channelized alluvial landscape coincide with deposition of Qt5 and Qt6 units in a second, incisional phase. All units consist of multiple 1-3 m thick alluvial packages deposited as upper-flow stage beds that represent individual storms. Main aggradational units (Qt2-Qt4) occurred across broad (>2 km) channels in the form of sheetflood deposition while incisional stage deposits are confined to channels of similar to 0.5 -2 km width. Continuous deposition inside the thicker (>10 m) pre-Qt5 units is demonstrated by closely spaced dates in vertical profiles. In a few places, disconformities between these major units are nevertheless evident and indicated by partly eroded buried soils. The described units feature sedimentological traits similar to historical deposits formed by large tropical cyclone events, but also include characteristics of upper-regime flow sedimentation not shown by historical sediments, like long (>10 m) wavelength antidunes and transverse ribs. We interpret the whole sequence as indicating discrete periods during the late Pleistocene and Holocene when climatic conditions allowed larger and more frequent tropical cyclone events than those observed historically. These discrete periods are associated with times when insolation at the tropics was higher than the present-day conditions, determined by precessional cycles, and modulated by the presence of El Nino-like conditions along the tropical and northeastern Pacific. The southern Baja California alluvial record is the first to document a precession-driven alluvial chronology for the region, and it constitutes a strong benchmark for discrimination of direct tropical influence on any other alluvial record in southwestern North America. (C) 2016 Elsevier Ltd. All rights reserved.

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