Daniel Muhs
I study geomorphology, soils and Quaternary stratigraphy to reconstruct paleoclimates over the past two and a half million years of geologic time.
My main study areas are in the central and western USA (Mississippi Valley, Great Plains, Rocky Mountains, desert Southwest, Pacific Coast and Alaska), but I have also worked in the Caribbean, Spain and Israel. My main interests are in origin and paleoclimatic significance of dune fields, stratigraphy and paleopedology of loess, effects of long-range-transported dust on soils, the atmosphere, oceans and ecosystems, and sea level history.
Education:
University of Colorado, Boulder, Colorado 1977-1980 (Ph.D., Physical geography/Geology)
University of Illinois, Urbana, Illinois 1973-1975 (M.S., Physical geography/Soil science)
University of Illinois, Urbana, Illinois 1972-1973 (B.A., Physical geography)
University of Illinois, Urbana, Illinois 1970-1972 (B.A., English, History)
Iowa State University, Ames, Iowa 1968-1970 (English)
Professional experience:
1995-date: Geologist, Geology and Environmental Change Science Center, USGS, Denver, CO
1985-1995: Geologist, Branch of Isotope Geology, USGS, Denver, CO
1983-1984: Soil Scientist with USGS while on leave-of-absence with the University of Wisconsin to accept National Research Council Research Associateship, Denver, Colorado.
1980-1985: Assistant and Associate Professor of Geography, University of Wisconsin, Madison, WI
1978-1980, part-time Soil Scientist, U.S. Geological Survey, Branch of Central Regional Geology.
1977-1979: Instructor (while a Ph.D student), Department of Geography, University of Colorado at Boulder and University of Colorado at Denver
1975-1976: Soil Scientist, U.S. Soil Conservation Service/Iowa State University
Science and Products
Chronology and provenance of last-glacial (Peoria) loess in western Iowa and paleoclimatic implications
Radiocarbon dating late Quaternary loess deposits using small terrestrial gastropod shells
Origin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history
The geologic records of dust in the Quaternary
From the Island of the Blue Dolphins: A unique 19th century cache feature from San Nicolas Island, California
Loess and its geomorphic, stratigraphic and paleoclimatic significance in the Quaternary
The contributions of Donald Lee Johnson to understanding the Quaternary geologic and biogeographic history of the California Channel Islands
Tectonic influences on the preservation of marine terraces: Old and new evidence from Santa Catalina Island, California
Soil genesis on the island of Bermuda in the Quaternary: the importance of African dust transport and deposition
Sea-level history of past interglacial periods: New evidence from uranium-series dating of corals from Curaçao, Leeward Antilles islands
Sea-level history during the Last Interglacial complex on San Nicolas Island, California: implications for glacial isostatic adjustment processes, paleozoogeography and tectonics
Duststones on Mars: Source, transport, deposition and erosion
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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Filter Total Items: 153
Chronology and provenance of last-glacial (Peoria) loess in western Iowa and paleoclimatic implications
Geologic archives show that the Earth was dustier during the last glacial period. One model suggests that increased gustiness (stronger, more frequent winds) enhanced dustiness. We tested this at Loveland, Iowa, one of the thickest deposits of last-glacial-age (Peoria) loess in the world. Based on K/Rb and Ba/Rb, loess was derived not only from glaciogenic sources of the Missouri River, but also dAuthorsDaniel R. Muhs, E. Arthur Bettis, Helen M. Roberts, Stephen S. Harlan, James B. Paces, Richard L. ReynoldsRadiocarbon dating late Quaternary loess deposits using small terrestrial gastropod shells
Constraining the ages and mass accumulation rates of late Quaternary loess deposits is often difficult because of the paucity of organic material typically available for 14C dating and the inherent limitations of luminescence techniques. Radiocarbon dating of small terrestrial gastropod shells may provide an alternative to these methods as fossil shells are common in loess and contain ∼12% carbonAuthorsJeff S. Pigati, John P. McGeehin, Daniel R. Muhs, E. Arthur BettisOrigin of the Sinai-Negev erg, Egypt and Israel: mineralogical and geochemical evidence for the importance of the Nile and sea level history
The Sinai–Negev erg occupies an area of 13,000 km2 in the deserts of Egypt and Israel. Aeolian sand of this erg has been proposed to be derived from the Nile Delta, but empirical data supporting this view are lacking. An alternative source sediment is sand from the large Wadi El Arish drainage system in central and northern Sinai. Mineralogy of the Negev and Sinai dunes shows that they are high inAuthorsDaniel R. Muhs, Joel Roskin, Haim Tsoar, Gary Skipp, James R. Budahn, Amihai Sneh, Naomi Porat, Jean-Daniel Stanley, Itzhak Katra, Dan G. BlumbergThe geologic records of dust in the Quaternary
Study of geologic records of dust composition, sources and deposition rates is important for understanding the role of dust in the overall planetary radiation balance, fertilization of organisms in the world’s oceans, nutrient additions to the terrestrial biosphere and soils, and for paleoclimatic reconstructions. Both glacial and non-glacial processes produce fine-grained particles that can be trAuthorsDaniel R. MuhsFrom the Island of the Blue Dolphins: A unique 19th century cache feature from San Nicolas Island, California
A cache feature salvaged from an eroding sea cliff on San Nicolas Island produced two redwood boxes containing more than 200 artifacts of Nicoleño, Native Alaskan, and Euro-American origin. Outside the boxes were four asphaltum-coated baskets, abalone shells, a sandstone dish, and a hafted stone knife. The boxes, made from split redwood planks, contained a variety of artifacts and numerous unmodifAuthorsJon M. Erlandson, Lisa Thomas-Barnett, René L. Vellanoweth, Steven J. Schwartz, Daniel R. MuhsLoess and its geomorphic, stratigraphic and paleoclimatic significance in the Quaternary
Loess is aeolian silt visible in the field as a sedimentary body. It covers a significant portion of the land surface of the Earth. Loess thickness, particle size, and carbonate content decrease downwind from sources, useful trends for paleowinds. Many loess sections consist of relatively thick deposits of mostly unaltered sediment with intercalated paleosols. Paleosols represent periods of landscAuthorsDaniel R. MuhsThe contributions of Donald Lee Johnson to understanding the Quaternary geologic and biogeographic history of the California Channel Islands
Over a span of 50 years, native Californian Donald Lee Johnson made a number of memorable contributions to our understanding of the California Channel Islands. Among these are (1) recognizing that carbonate dunes, often cemented into eolianite and derived from offshore shelf sediments during lowered sea level, are markers of glacial periods on the Channel Islands; (2) identifying beach rock on theAuthorsDaniel R. MuhsTectonic influences on the preservation of marine terraces: Old and new evidence from Santa Catalina Island, California
The California Channel Islands contain some of the best geologic records of past climate and sea-level changes, recorded in uplifted, fossil-bearing marine terrace deposits. Among the eight California Channel Islands and the nearby Palos Verdes Hills, only Santa Catalina Island does not exhibit prominent emergent marine terraces, though the same terrace-forming processes that acted on the other ChAuthorsR. Randall Schumann, Scott A. Minor, Daniel R. Muhs, Lindsey T. Groves, John P. McGeehinSoil genesis on the island of Bermuda in the Quaternary: the importance of African dust transport and deposition
The origin of terra rossa, red or reddish-brown, clay-rich soils overlying high-purity carbonate substrates, has intrigued geologists and pedologists for decades. Terra rossa soils can form from accumulation of insoluble residues during dissolution of the host limestones, addition of volcanic ash, or addition of externally derived, long-range-transported (LRT) aeolian particles. We studied soils aAuthorsDaniel R. Muhs, James R. Budahn, Joseph M. Prospero, Gary Skipp, Stanley R. HerwitzSea-level history of past interglacial periods: New evidence from uranium-series dating of corals from Curaçao, Leeward Antilles islands
Curaçao has reef terraces with the potential to provide sea-level histories of interglacial periods. Ages of the Hato (upper) unit of the “Lower Terrace” indicate that this reef dates to the last interglacial period, Marine Isotope Stage (MIS) 5.5. On Curaçao, this high sea stand lasted at least 8000 yr (~ 126 to ~ 118 ka). Elevations and age of this reef show that late Quaternary uplift rates onAuthorsDaniel R. Muhs, John M. Pandolfi, Kathleen R. Simmons, R. Randall SchumannSea-level history during the Last Interglacial complex on San Nicolas Island, California: implications for glacial isostatic adjustment processes, paleozoogeography and tectonics
San Nicolas Island, California has one of the best records of fossiliferous Quaternary marine terraces in North America, with at least fourteen terraces rising to an elevation of ~270 m above present-day sea level. In our studies of the lowest terraces, we identified platforms at 38-36 m (terrace 2a), 33-28 m (terrace 2b), and 13-8 m (terrace 1). Uranium-series dating of solitary corals from theseAuthorsDaniel R. Muhs, Kathleen R. Simmons, R. Randall Schumann, Lindsey T. Groves, Jerry X. Mitrovica, Deanna LaurelDuststones on Mars: Source, transport, deposition and erosion
Dust is an abundant material on Mars, and there is strong evidence that it is a contributor to the rock record as “duststone,” analogous in many ways to loess on Earth. Although a common suite of dust formation mechanisms has operated on the two planets, fundamental differences in environments and geologic histories have resulted in vastly different weighting functions, causing distinct depositionAuthorsNathan T. Bridges, Daniel R. MuhsNon-USGS Publications**
Crittenden, R.C. and Muhs, D.R., 1986, Cliff-height and slope-angle relationships in a chronosequence of marine terraces, San Clemente Island, California: Zeitschrift für Geomorphologie, v. 30, p. 291-301.Muhs, D.R., 1985, Age and paleoclimatic significance of Holocene sand dunes in northeastern Colorado: Annals of the Association of American Geographers, v. 75, p. 566-582.Muhs, D.R., 1985, Amino acid age estimates of marine terraces and sea levels, San Nicolas Island, California: Geology, v. 13, p. 58-61.Muhs, D.R., Kautz, R., and MacKinnon, J.J., 1985, Soils and the location of cacao orchards at a Maya site in western Belize: Journal of Archaeological Science, v. 12, p. 121-137.Muhs, D.R., 1984, Intrinsic thresholds in soil systems: Physical Geography, v. 5, p. 99-110.Muhs, D.R., 1983, Airborne dust fall on the California Channel Islands, U.S.A.: Journal of Arid Environments, v. 6, p. 223-238.Muhs, D.R., 1983, Quaternary sea-level events on northern San Clemente Island, California: Quaternary Research, v. 20, p. 322-341.Gillette, D.A., Adams, J., Muhs, D.R., and Kihl, R., 1982, Threshold friction velocities and rupture moduli for crusted desert soils for the input of soil particles into the air: Journal of Geophysical Research, v. 87, p. 9003-9015.
Muhs, D.R., 1982, A soil chronosequence on Quaternary marine terraces, San Clemente Island, California: Geoderma, v. 28, p. 257-283.Muhs, D.R. and Szabo, B.J., 1982, Uranium-series age of the Eel Point terrace, San Clemente Island, California: Geology, v. 10, p. 23-26.Muhs, D.R., 1982, The influence of topography on the spatial variability of soils in Mediterranean climates, in Thorn, C.E., ed., Space and Time in Geomorphology: London, George Allen and Unwin, p. 269-284.Johnson, D.L., Muhs, D.R., and Barnhardt, M.L., 1977, The effects of frost heaving on objects in soils, II: Laboratory experiments: Plains Anthropologist, v. 22, p. 133-147.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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