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Journal articles on the topic 'Paleomagnetism – California – Mojave Desert'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

MacFadden, Bruce J., Michael O. Woodburne, and Neil D. Opdyke. "Paleomagnetism and Neogene clockwise rotation of the Northern Cady Mountains, Mojave Desert of southern California." Journal of Geophysical Research 95, B4 (1990): 4597. http://dx.doi.org/10.1029/jb095ib04p04597.

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2

MAcFADDEN, BRUCE J., CARL C. SWISHER III, NEIL D. OPDYKE, and MICHAEL O. WOODBURNE. "Paleomagnetism, geochronology, and possible tectonic rotation of the middle Miocene Barstow Formation, Mojave Desert, southern California." Geological Society of America Bulletin 102, no. 4 (1990): 478–93. http://dx.doi.org/10.1130/0016-7606(1990)102<0478:pgaptr>2.3.co;2.

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3

Calderone, Gary J., Robert F. Butler, and Gary D. Acton. "Paleomagnetism of Middle Miocene volcanic rocks in the Mojave-Sonora Desert region of western Arizona and southeastern California." Journal of Geophysical Research 95, B1 (1990): 625. http://dx.doi.org/10.1029/jb095ib01p00625.

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4

Valentine, Michael J., Laurie L. Brown, and Matthew P. Golombek. "Cenozoic crustal rotations in the Mojave Desert from paleomagnetic studies around Barstow, California." Tectonics 12, no. 3 (1993): 666–77. http://dx.doi.org/10.1029/92tc02813.

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5

Ross, Timothy M., Bruce P. Luyendyk, and Roger B. Haston. "Paleomagnetic evidence for Neogene clockwise tectonic rotations in the central Mojave Desert, California." Geology 17, no. 5 (1989): 470. http://dx.doi.org/10.1130/0091-7613(1989)017<0470:pefnct>2.3.co;2.

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6

Sabbeth, Leah, Brian P. Wernicke, Timothy D. Raub, Jeffrey A. Grover, E. Bruce Lander, and Joseph L. Kirschvink. "Grand Canyon provenance for orthoquartzite clasts in the lower Miocene of coastal southern California." Geosphere 15, no. 6 (2019): 1973–98. http://dx.doi.org/10.1130/ges02111.1.

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Abstract Orthoquartzite detrital source regions in the Cordilleran interior yield clast populations with distinct spectra of paleomagnetic inclinations and detrital zircon ages that can be used to trace the provenance of gravels deposited along the western margin of the Cordilleran orogen. An inventory of characteristic remnant magnetizations (CRMs) from >700 sample cores from orthoquartzite source regions defines a low-inclination population of Neoproterozoic–Paleozoic age in the Mojave Desert–Death Valley region (and in correlative strata in Sonora, Mexico) and a moderate- to high-inclina

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7

MacConnell, D. F., C. McCabe, R. K. Dokka, and M. Chu. "Paleomagnetic and structural evidence for localized tectonic rotation associated with fault drag in the northeastern Mojave Desert: Implications for the late Cenozoic tectonic evolution of the Eastern California shear zone." Earth and Planetary Science Letters 126, no. 4 (1994): 207–16. http://dx.doi.org/10.1016/0012-821x(94)90107-4.

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8

Laity, Julie E. "TOPOGRAPHIC EFFECTS ON VENTIFACT DEVELOPMENT, MOJAVE DESERT, CALIFORNIA." Physical Geography 8, no. 2 (1987): 113–32. http://dx.doi.org/10.1080/02723646.1987.10642315.

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9

Garcia, Anna L., Jeffrey R. Knott, Shannon A. Mahan, and Jordon Bright. "Geochronology and paleoenvironment of pluvial Harper Lake, Mojave Desert, California, USA." Quaternary Research 81, no. 2 (2014): 305–17. http://dx.doi.org/10.1016/j.yqres.2013.10.008.

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AbstractAccurate reconstruction of the paleo-Mojave River and pluvial lake (Harper, Manix, Cronese, and Mojave) system of southern California is critical to understanding paleoclimate and the North American polar jet stream position over the last 500 ka. Previous studies inferred a polar jet stream south of 35°N at 18 ka and at ~ 40°N at 17–14 ka. Highstand sediments of Harper Lake, the upstream-most pluvial lake along the Mojave River, have yielded uncalibrated radiocarbon ages ranging from 24,000 to > 30,000 14C yr BP. Based on geologic mapping, radiocarbon and optically stimulated lumine

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10

Alagona, Peter S., and Clinton F. Smith. "Mirage in the Making." Boom 2, no. 3 (2012): 25–44. http://dx.doi.org/10.1525/boom.2012.2.3.25.

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The Mojave Desert in California is undergoing a boom in renewable energy, mostly in the form of utility-scale solar power plants. These projects have met with resistance from diverse groups concerned about impacts on desert landscapes, ecosystems, water resources, archaeological sites, military training exercises, and other natural and cultural resources and land uses. This paper explores the current debate over renewable energy in the Mojave in the context of the region’s broader environmental history. What do Californians want from the Mojave Desert? We conclude that residents of the state w

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11

Boettcher, Stefan S., and J. Douglas Walker. "Geologic evolution of Iron Mountain, central Mojave Desert, California." Tectonics 12, no. 2 (1993): 372–86. http://dx.doi.org/10.1029/92tc02423.

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12

Hooke, Roger LeB. "Lake Manly(?) Shorelines in the Eastern Mojave Desert, California." Quaternary Research 52, no. 3 (1999): 328–36. http://dx.doi.org/10.1006/qres.1999.2080.

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Near Mesquite Spring on the southern edge of the Soda Lake basin in the Mojave Desert, there is a shoreline of an ancient lake at an elevation of 340 m above sea level. At present, Soda Lake would overflow at 280 m; a lake surface at 340 m would extend ∼240 km northward, to the northern end of Death Valley. Shorelines and lacustrine deposits near the Salt Spring and Saddle Peak Hills, 75 km north of Mesquite Spring, are at ∼180 m; a lake surface at this elevation today would also extend to the northern end of Death Valley. The most prominent shoreline of the pluvial lake that occupied Death Va

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13

Lovich, Jeffrey E., George Jefferson, Robert Reynolds, et al. "Western pond turtles in the Mojave Desert? A review of their past, present, and possible future." Vertebrate Zoology 71 (May 25, 2021): 317–34. http://dx.doi.org/10.3897/vz.71.e63987.

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The western pond turtle (WPT) was formerly considered a single species (Actinemys or Emys marmorata) that ranged from southern British Columbia, Canada to Baja California, México. More recently it was divided into a northern and a southern species. WPTs are found primarily in streams that drain into the Pacific Ocean, although scattered populations exist in endorheic drainages of the Great Basin and Mojave deserts. Populations in the Mojave Desert were long thought to be restricted to the Mojave River, but recently another population was documented in Piute Ponds, a terminal wetland complex as

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14

Anderson, K., S. Wells, and R. Graham. "Pedogenesis of Vesicular Horizons, Cima Volcanic Field, Mojave Desert, California." Soil Science Society of America Journal 66, no. 3 (2002): 878. http://dx.doi.org/10.2136/sssaj2002.0878.

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15

Anderson, K., S. Wells, and R. Graham. "Pedogenesis of Vesicular Horizons, Cima Volcanic Field, Mojave Desert, California." Soil Science Society of America Journal 66, no. 3 (2002): 878–87. http://dx.doi.org/10.2136/sssaj2002.8780.

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16

Dokka, Roy K., and Christopher J. Travis. "Late Cenozoic strike-slip faulting in the Mojave Desert, California." Tectonics 9, no. 2 (1990): 311–40. http://dx.doi.org/10.1029/tc009i002p00311.

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17

Sauber, Jeanne, Wayne Thatcher, and Sean C. Solomon. "Geodetic measurement of deformation in the central Mojave Desert, California." Journal of Geophysical Research: Solid Earth 91, B12 (1986): 12683–93. http://dx.doi.org/10.1029/jb091ib12p12683.

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18

Cole, Kenneth L., and Robert H. Webb. "Late Holocene Vegetation Changes in Greenwater Valley, Mojave Desert, California." Quaternary Research 23, no. 2 (1985): 227–35. http://dx.doi.org/10.1016/0033-5894(85)90030-4.

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Small-scale late Holocene vegetation changes were determined from a series of 13 modern and fossil packrat middens collected from a site in the Greenwater Valley, northern Mojave Desert, California. Although the site is above the modern lower limit ofColeogyne ramosissima(black-brush), macrofossils of this shrub are only present in samples younger than 270 yr B.P. In order to measure changes more subtle than presence vs absence, macrofossil concentrations were quantified, and principal components and factor analyses were used to distinguish midden plant assemblages. Both the presence/absence d

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19

Kelly, Erica C., Brian L. Cypher, and David J. Germano. "Exploitative competition between desert kit foxes and coyotes in the Mojave Desert." Pacific Conservation Biology 26, no. 1 (2020): 57. http://dx.doi.org/10.1071/pc19007.

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Exploitative competition between two sympatric guild members can influence the composition and dynamics of an ecological community. We assessed potential exploitative competition between desert kit foxes (Vulpes macrotis arsipus) and coyotes (Canis latrans) by comparing food habits of the two species from 2009 to 2014 on a study site in the Mojave Desert in California. Desert kit foxes specialised on heteromyid rodents and invertebrates, while the most frequently occurring items consumed by coyotes were lagomorphs and rodents. Both species consumed a variety of food items throughout the study,

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20

Schelble, Rachel T., Gene D. McDonald, James A. Hall, and Kenneth H. Nealson. "Community Structure Comparison Using FAME Analysis of Desert Varnish and Soil, Mojave Desert, California." Geomicrobiology Journal 22, no. 7-8 (2005): 353–60. http://dx.doi.org/10.1080/01490450500248754.

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21

Laity, Julie. "Aeolian Destabilization Along the Mojave River, Mojave Desert, California: Linkages Among Fluvial, Groundwater, and Aeolian Systems." Physical Geography 24, no. 3 (2003): 196–221. http://dx.doi.org/10.2747/0272-3646.24.3.196.

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22

Goodwin, H. Thomas, and Robert E. Reynolds. "Late Quaternary Sciuridae from Low Elevations in the Mojave Desert, California." Southwestern Naturalist 34, no. 4 (1989): 506. http://dx.doi.org/10.2307/3671509.

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23

Goodwin, H. Thomas. "Marmota flaviventris from the Central Mojave Desert of California: Biogeographic Implications." Southwestern Naturalist 34, no. 2 (1989): 284. http://dx.doi.org/10.2307/3671741.

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24

Eghbal, Mostafa K., and Randal J. Southard. "Mineralogy of Aridisols on Dissected Alluvial Fans, Western Mojave Desert, California." Soil Science Society of America Journal 57, no. 2 (1993): 538–44. http://dx.doi.org/10.2136/sssaj1993.03615995005700020040x.

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25

Eghbal, Mostafa K., and Randal J. Southard. "Micromorphological Evidence of Polygenesis of Three Aridisols, Western Mojave Desert, California." Soil Science Society of America Journal 57, no. 4 (1993): 1041–50. http://dx.doi.org/10.2136/sssaj1993.03615995005700040027x.

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26

Webb, Robert H., John W. Steiger, and Raymond M. Turner. "Dynamics of Mojave Desert Shrub Assemblages in the Panamint Mountains, California." Ecology 68, no. 3 (1987): 478–90. http://dx.doi.org/10.2307/1938453.

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27

Prose, D. V., Susan K. Metzger, and H. G. Wilshire. "Effects of Substrate Disturbance on Secondary Plant Succession; Mojave Desert, California." Journal of Applied Ecology 24, no. 1 (1987): 305. http://dx.doi.org/10.2307/2403806.

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28

Louie, John N., and Robert W. Clayton. "The nature of deep crustal structures in the Mojave Desert, California." Geophysical Journal International 89, no. 1 (1987): 125–32. http://dx.doi.org/10.1111/j.1365-246x.1987.tb04398.x.

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29

Pollitz, Fred F. "Transient rheology of the uppermost mantle beneath the Mojave Desert, California." Earth and Planetary Science Letters 215, no. 1-2 (2003): 89–104. http://dx.doi.org/10.1016/s0012-821x(03)00432-1.

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30

De Ley, Irma, James Baldwin, Paul De Ley, Manuel Mundo-Ocampo, Steven Nadler, and Michael Gebre. "Acromoldavicus mojavicus n. sp. (Nematoda: Cephaloboidea) from the Mojave Desert, California." Nematology 3, no. 4 (2001): 343–53. http://dx.doi.org/10.1163/156854101317020268.

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AbstractAcromoldavicus (Cephalobina, Cephaloboidea) with its highly distinctive lip region has only a single species, Acromoldavicus skrjabini Nesterov & Lisetskaya, originally described from Moldova and subsequently also detected at sites in the Middle East and near the Mediterranean. Herein, Acromoldavicus mojavicus n. sp. is described from sandy soil surrounding a Joshua tree (Yucca brevifolia) in a remote area of the Mojave Desert, California, USA. The lip region of A. mojavicus n. sp. is bilaterally symmetrical with three triangular probolae surrounded by three pairs of plate-like lip

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31

King, N. E. "Horizontal deformation in the Mojave Desert near Barstow, California, 1979-1983." Journal of Geophysical Research: Solid Earth 90, B6 (1985): 4491–94. http://dx.doi.org/10.1029/jb090ib06p04491.

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32

Webb, Robert H. "Recovery of Severely Compacted Soils in the Mojave Desert, California, USA." Arid Land Research and Management 16, no. 3 (2002): 291–305. http://dx.doi.org/10.1080/153249802760284829.

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33

Miller, Jonathan S., and Allen F. Glazner. "Jurassic plutonism and crustal evolution in the central Mojave Desert, California." Contributions to Mineralogy and Petrology 118, no. 4 (1995): 379–95. http://dx.doi.org/10.1007/s004100050021.

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34

Aguado, Edward. "Effect of advected pollutants on solar radiation attenuation: Mojave Desert, California." Atmospheric Environment. Part B. Urban Atmosphere 24, no. 1 (1990): 153–57. http://dx.doi.org/10.1016/0957-1272(90)90020-u.

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35

Schlesinger, William H. "The formation of caliche in soils of the Mojave Desert, California." Geochimica et Cosmochimica Acta 49, no. 1 (1985): 57–66. http://dx.doi.org/10.1016/0016-7037(85)90191-7.

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36

GRISWOLD, TERRY, and WENSDAE MILLER. "A Revision of Perdita (Xerophasma) Timberlake (Hymenoptera: Andrenidae)." Zootaxa 2517, no. 1 (2010): 1. http://dx.doi.org/10.11646/zootaxa.2517.1.1.

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Three new species of Perdita (Xerophasma) endemic to the Mojave Desert are described: P. celadona Griswold and Miller and P. vespertina Griswold and Miller from eastern Clark County, Nevada, and P. rhondae Griswold from Death Valley, California. The subgenus is redescribed to accommodate these new species. New distributional records for P. bequaertiana and P. pallida and a key to the species of the subgenus are provided. A well supported phylogeny suggests evolution toward nocturnal foraging expressed in increasing ocellar size and a trend toward totally pale integument. The apparent origin an

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37

Schmid, Rudolf, and Jon Mark Stewart. "Mojave Desert Wildflowers: A Field Guide to High Desert Wildflowers of California, Nevada, and Arizona." Taxon 47, no. 3 (1998): 785. http://dx.doi.org/10.2307/1223625.

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38

Berry, K. H., T. Y. Bailey, and K. M. Anderson. "Attributes of desert tortoise populations at the National Training Center, Central Mojave Desert, California, USA." Journal of Arid Environments 67 (January 2006): 165–91. http://dx.doi.org/10.1016/j.jaridenv.2006.09.026.

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39

Wells, Stephen G., Leslie D. McFadden, and John C. Dohrenwend. "Influence of Late Quaternary Climatic Changes on Geomorphic and Pedogenic Processes on a Desert Piedmont, Eastern Mojave Desert, California." Quaternary Research 27, no. 2 (1987): 130–46. http://dx.doi.org/10.1016/0033-5894(87)90072-x.

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AbstractRadiocarbon dating of late Quaternary deposits and shorelines of Lake Mojave and cation-ratio numerical age dating of stone pavements (Dorn, 1984) on the adjacent Soda Mountains piedmont provide age constraints for alluvial and eolian deposits. These deposits are associated with climatically controlled stands of Lake Mojave during the past 15,000 yr. Six alluvial fan units and three eolian stratigraphic units were assigned ages based on field relations with dated shorelines and piedmont surfaces, as well as on soil-geomorphic data. All but one of these stratigraphic units were deposite

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40

Grodsky, Steven, Leslie Saul-Gershenz, Kara Moore-O’Leary, and Rebecca Hernandez. "Her Majesty’s Desert Throne: The Ecology of Queen Butterfly Oviposition on Mojave Milkweed Host Plants." Insects 11, no. 4 (2020): 257. http://dx.doi.org/10.3390/insects11040257.

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Butterfly–host plant relationships can inform our understanding of ecological and trophic interactions that contribute to ecosystem function, resiliency, and services. The ecology of danaid–milkweed (Apocynaceae) host plant interactions has been studied in several biomes but is neglected in deserts. Our objective was to determine effects of plant traits, seasonality, and landscape-level host plant availability on selection of Mojave milkweed (Asclepias nyctaginifolia A. Gray) by ovipositing monarch butterflies (Danaus plexippus plexippus) and queen butterflies (Danaus gilippus thersippus) in t

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41

Sweeney, Mark R., Eric V. McDonald, Lucas P. Chabela, and Paul R. Hanson. "The role of eolian-fluvial interactions and dune dams in landscape change, late Pleistocene–Holocene, Mojave Desert, USA." GSA Bulletin 132, no. 11-12 (2020): 2318–32. http://dx.doi.org/10.1130/b35434.1.

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Abstract The formation of the Kelso Dunes in the eastern Mojave Desert, California, was a landscape-changing event triggered by an increase in sediment supply that followed the incision of Afton Canyon by the Mojave River ca. 25 ka. Eastward migration of sand dunes occurred along a well-defined eolian transport corridor. Dunes temporarily blocked washes resulting in substantial aggradation of eolian and fluvial sediments. Stratigraphic exposures reveal numerous fining-up sequences with interbedded eolian sands that provide evidence of dune dams and subsequent aggradation. Luminescence ages rev

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42

LOUGHNEY, KATHARINE M., and CATHERINE BADGLEY. "FACIES, ENVIRONMENTS, AND FOSSIL PRESERVATION IN THE BARSTOW FORMATION, MOJAVE DESERT, CALIFORNIA." PALAIOS 32, no. 6 (2017): 396–412. http://dx.doi.org/10.2110/palo.2017.008.

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43

Eerkens, Jelmer W., Jeffrey S. Rosenthal, D. Craig Young, and Jay King. "Early Holocene Landscape Archaeology in the Coso Basin, Northwestern Mojave Desert, California." North American Archaeologist 28, no. 2 (2007): 87–112. http://dx.doi.org/10.2190/na.28.2.a.

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44

Dokka, Roy K., and Kristine Y. Macaluso. "Topographic effects of the Eastern California Shear Zone in the Mojave Desert." Journal of Geophysical Research: Solid Earth 106, B12 (2001): 30625–44. http://dx.doi.org/10.1029/2000jb000017.

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45

Miller, Jonathan S., and Calvin F. Miller. "Tertiary extension-related volcanism, Old Woman Mountains area eastern Mojave Desert, California." Journal of Geophysical Research: Solid Earth 96, B8 (1991): 13629–43. http://dx.doi.org/10.1029/91jb00607.

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46

HANCHAR, J. M., C. F. MILLER, J. L. WOODEN, V. C. BENNETT, and J. M. G. STAUDE. "Evidence from Xenoliths for a Dynamic Lower Crust, Eastern Mojave Desert, California." Journal of Petrology 35, no. 5 (1994): 1377–415. http://dx.doi.org/10.1093/petrology/35.5.1377.

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47

Farr, Tom G. "Microtopographic evolution of lava flows at Cima Volcanic Field, Mojave Desert, California." Journal of Geophysical Research 97, B11 (1992): 15171. http://dx.doi.org/10.1029/92jb01592.

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48

WOODBURNE, MICHAEL O., RICHARD H. TEDFORD, and CARL C. SWISHER III. "Lithostratigraphy, biostratigraphy, and geochronology of the Barstow Formation, Mojave Desert, southern California." Geological Society of America Bulletin 102, no. 4 (1990): 459–77. http://dx.doi.org/10.1130/0016-7606(1990)102<0459:lbagot>2.3.co;2.

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49

James, W. C., Martin A. Knoll, and Kevin L. Mickus. "Ship Mountains Megabreccia: Implications for Miocene Extensional Tectonics, Eastern Mojave Desert, California." Journal of Geology 101, no. 1 (1993): 115–20. http://dx.doi.org/10.1086/648200.

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50

Groover, Krishangi D., and John A. Izbicki. "Selected trace-elements in alluvium and rocks, western Mojave Desert, southern California." Journal of Geochemical Exploration 200 (May 2019): 234–48. http://dx.doi.org/10.1016/j.gexplo.2018.09.005.

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