Hostname: page-component-669899f699-7xsfk Total loading time: 0 Render date: 2025-04-26T15:12:30.179Z Has data issue: false hasContentIssue false
  • English
  • Français

The role of lithology and climate on bedrock river incision and terrace development along the Buffalo National River, Arkansas

Published online by Cambridge University Press:  26 May 2023

Kathleen Rodrigues Open the ORCID record for Kathleen Rodrigues [Opens in a new window] ,
Amanda Keen-Zebert ,
Stephanie Shepherd ,
Mark R. Hudson ,
Charles J. Bitting ,
Bradley G. Johnson  and
Abigail Langston
Kathleen Rodrigues*
Affiliation:
Division of Earth and Ecosystem Sciences, Desert Research Institute, Reno, Nevada, USA, 86512
Amanda Keen-Zebert
Affiliation:
Division of Earth and Ecosystem Sciences, Desert Research Institute, Reno, Nevada, USA, 86512
Stephanie Shepherd
Affiliation:
Department of Geoscience, Auburn University, Auburn, Alabama, USA, 36849
Mark R. Hudson
Affiliation:
U.S. Geological Survey, Denver, Colorado, USA, 80225
Charles J. Bitting
Affiliation:
National Park Service, Buffalo National River, Harrison, Arkansas, USA, 72601
Bradley G. Johnson
Affiliation:
Environmental Studies Department, Davidson College, Davidson, North Carolina, USA, 28035
Abigail Langston
Affiliation:
Department of Geography and Geospatial Sciences, Kansas State University, Manhattan, Kansas, USA, 66506
*
*Corresponding author email address: <krodrigues@nevada.unr.edu>
Get access Rights & Permissions [Opens in a new window]

Abstract

The Buffalo National River in northwest Arkansas preserves an extensive Quaternary record of fluvial bedrock incision and aggradation across lithologies of variable resistance. In this work, we apply optically stimulated luminescence (OSL) dating to strath and fill terraces along the Buffalo River to elucidate the role of lithology and climate on the development of the two youngest terrace units (Qtm and Qty). Our OSL ages suggest a minimum strath planation age of ca. 250 ka for the Qtm terraces followed by a ca. 200 ka record of aggradation. Qtm incision likely occurred near the last glacial maximum (LGM), prior to the onset of Qty fill terrace aggradation ca. 14 ka. Our terrace ages are broadly consistent with other regional terrace records, and comparison with available paleoclimatic archives suggests that terrace aggradation and incision occurred during drier and wetter hydrological conditions, respectively. Vertical bedrock incision rates were also calculated using OSL-derived estimates of Qtm strath planation and displayed statistically significant spatial variability with bedrock lithology, ranging from ~35 mm/ka in the higher resistance reaches and ~16 mm/ka in the lower resistance reaches. In combination with observations of valley width and terrace distribution, these results suggest that vertical processes outpace lateral ones in lithologic reaches with higher resistance.

Keywords

Strath terracesGeochronologyOSL datingPaleoclimateBedrock riversGeomorphology
Type
Research Article
Information
Quaternary Research , Volume 115 , September 2023 , pp. 179 - 193
Check for updates
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2023

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

REFERENCES

Aitken, M.J., 1998. Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-stimulated Luminescence. Clarendon Press, Oxford, UK.Google Scholar
Anthony, D.M., Granger, D.E., 2007. A new chronology for the age of Appalachian erosional surfaces determined by cosmogenic nuclides in cave sediments. Earth Surface Processes and Landforms 32, 874–887.CrossRefGoogle Scholar
Arnold, L.J., Demuro, M., 2015. Insights into TT-OSL signal stability from single-grain analyses of known-age deposits at Atapuerca, Spain. Quaternary Geochronology 30, 472–478.CrossRefGoogle Scholar
Bateman, M.D., Boulter, C.H., Carr, A.S., Frederick, C.D., Peter, D., Wilder, M., 2007. Detecting post-depositional sediment disturbance in sandy deposits using optical luminescence. Quaternary Geochronology 2, 57–64.CrossRefGoogle Scholar
Beeson, H.W., McCoy, S.W., Keen-Zebert, A., 2017. Geometric disequilibrium of river basins produces long-lived transient landscapes. Earth and Planetary Science Letters 475, 34–43.CrossRefGoogle Scholar
Bettis, E.A., III, Mandel, R.D., 2002. The effects of temporal and spatial patterns of Holocene erosion and alluviation on the archaeological record of the Central and Eastern Great Plains, USA. Geoarchaeology 17, 141–154.CrossRefGoogle Scholar
Bishop, P., Goldrick, G., 2010. Lithology and the evolution of bedrock rivers in post-orogenic settings: constraints from the high-elevation passive continental margin of SE Australia. Geological Society, London, Special Publications 346, 267–287.CrossRefGoogle Scholar
Blum, M.D., Price, D.M., 1998. Quaternary Alluvial Plain Construction in Response to Glacio-Eustatic and Climatic Controls, Texas Gulf Coastal Plain. In: Kocurek, G. (Ed.), Relative Role of Eustacy, Climate, and Tectonism in Continental Rocks. SEPM (Society for Sedimentary Geology). https://doi.org/10.2110/pec.98.59.0031.Google Scholar
Brakenridge, G.R., 1981. Late Quaternary floodplain sedimentation along the Pomme de Terre River, southern Missouri. Quaternary Research 15, 62–76.CrossRefGoogle Scholar
Bufe, A., Paola, C., Burbank, D.W., 2016. Fluvial bevelling of topography controlled by lateral channel mobility and uplift rate. Nature Geoscience 9, 706–710.CrossRefGoogle Scholar
Bull, W.B., 1990. Stream-terrace genesis: implications for soil development. Geomorphology 3, 351–367.CrossRefGoogle Scholar
Bull, W.B., 1991. Geomorphic Responses to Climatic Change. Oxford University Press, Oxford, UK.Google Scholar
Chandler, A.K., Ausbrooks, S.M., 2015a. Geologic map of the Mt. Judea quadrangle, Newton County, Arkansas. Arkansas Geological Survey Digital Geologic Quadrangle Map DGM-AR-00590, 1:24,000 scale. https://www.geology.arkansas.gov/docs/pdf/maps-and-data/geologic_maps/24k/Mount%20Judea.pdf.Google Scholar
Chandler, A.K., Ausbrooks, S.M., 2015b. Geologic map of the Snowball quadrangle, Searcy County, Arkansas. Arkansas Geological Survey Digital Geologic Quadrangle Map DGM-AR-00800, 1:24,000 scale. https://www.geology.arkansas.gov/docs/pdf/maps-and-data/geologic_maps/24k/Snowball.pdf.Google Scholar
Chapot, M., Roberts, H., Duller, G., Lai, Z., 2016. Natural and laboratory TT-OSL dose response curves: testing the lifetime of the TT-OSL signal in nature. Radiation Measurements 85, 41–50.CrossRefGoogle Scholar
Cook, K.L., Whipple, K.X., Heimsath, A.M., Hanks, T.C., 2009. Rapid incision of the Colorado River in Glen Canyon—insights from channel profiles, local incision rates, and modeling of lithologic controls. Earth Surface Processes and Landforms 34, 994–1010.Google Scholar
Covington, M.D., Gulley, J.D., Gabrovšek, F., 2015. Natural variations in calcite dissolution rates in streams: controls, implications, and open questions. Geophysical Research Letters 42, 2836–2843.CrossRefGoogle Scholar
Covington, M.D., Vaughn, K.A., 2019. Carbon dioxide and dissolution rate dynamics within a karst underflow-overflow system, Savoy Experimental Watershed, Arkansas, USA. Chemical Geology 527, 118689. https://doi.org/10.1016/j.chemgeo.2018.03.009.CrossRefGoogle Scholar
Croneis, C., 1930. Geology of the Arkansas Paleozoic area, with especial reference to oil and gas possibilities. Arkansas Geological Survey Bulletin 3, 1–457.Google Scholar
Delcourt, P.A., Delcourt, H.R., 1996. Quaternary paleoecology of the Lower Mississippi Valley. Engineering Geology 45, 219–242.CrossRefGoogle Scholar
Demuro, M., Arnold, L.J., Parés, J.M., Sala, R., 2015. Extended-range luminescence chronologies suggest potentially complex bone accumulation histories at the Early-to-Middle Pleistocene palaeontological site of Huéscar-1 (Guadix-Baza basin, Spain). Quaternary International 389, 191–212.CrossRefGoogle Scholar
Denniston, R.F., González, L.A., Asmerom, Y., Reagan, M.K., Recelli-Snyder, H., 2000. Speleothem carbon isotopic records of Holocene environments in the Ozark Highlands, USA. Quaternary International 67, 21–27.CrossRefGoogle Scholar
Denniston, R.F., Gonzalez, L.A., Semken, H.A., Asmerom, Y., Baker, R.G., Recelli-Snyder, H., Reagan, M.K., Bettis, E.A., 1999. Integrating stalagmite, vertebrate, and pollen sequences to investigate Holocene vegetation and climate change in the southern Midwestern United States. Quaternary Research 52, 381–387.CrossRefGoogle Scholar
DiBiase, R.A., Denn, A.R., Bierman, P.R., Kirby, E., West, N., Hidy, A.J., 2018. Stratigraphic control of landscape response to base-level fall, Young Womans Creek, Pennsylvania, USA. Earth and Planetary Science Letters 504, 163–173.CrossRefGoogle Scholar
Dorale, J.A., Edwards, R.L., Ito, E., González, L.A., 1998. Climate and vegetation history of the Midcontinent from 75 to 25 ka: a speleothem record from Crevice Cave, Missouri, USA. Science 282, 1871–1874.CrossRefGoogle Scholar
Duller, G.A.T., 2003. Distinguishing quartz and feldspar in single grain luminescence measurements. Radiation Measurements 37, 161–165.CrossRefGoogle Scholar
Duller, G., Wintle, A., 2012. A review of the thermally transferred optically stimulated luminescence signal from quartz for dating sediments. Quaternary Geochronology 7, 6–20.CrossRefGoogle Scholar
Faershtein, G., Guralnik, B., Lambert, R., Matmon, A., Porat, N., 2018. Investigating the thermal stability of TT-OSL main source trap. Radiation Measurements 119, 102–111.CrossRefGoogle Scholar
Finnegan, N.J., Dietrich, W.E., 2011. Episodic bedrock strath terrace formation due to meander migration and cutoff. Geology 39, 143–146.CrossRefGoogle Scholar
Finnegan, N.J., Schumer, R., Finnegan, S., 2014. A signature of transience in bedrock river incision rates over timescales of 104–107 years. Nature 505, 391–394.CrossRefGoogle Scholar
Forman, S.L., Marín, L., Gomez, J., Pierson, J., 2008. Late Quaternary eolian sand depositional record for southwestern Kansas: landscape sensitivity to droughts. Palaeogeography, Palaeoclimatology, Palaeoecology 265, 107–120.CrossRefGoogle Scholar
Forte, A.M., Yanites, B.J., Whipple, K.X., 2016. Complexities of landscape evolution during incision through layered stratigraphy with contrasts in rock strength. Earth Surface Processes and Landforms 41, 1736–1757.CrossRefGoogle Scholar
Foster, M.A., Anderson, R.S., Gray, H.J., Mahan, S.A., 2017. Dating of river terraces along Lefthand Creek, western High Plains, Colorado, reveals punctuated incision. Geomorphology 295, 176–190.CrossRefGoogle Scholar
Galbraith, R.F., Roberts, R.G., Laslett, G.M., Yoshida, H., Olley, J.M., 1999. Optical dating of single and multiple grains of quartz from Jinmium Rock Shelter, Northern Australia: part I, experimental design and statistical models. Archaeometry 41, 339–364.CrossRefGoogle Scholar
García, A.F., Mahan, S.A., 2014. The notion of climate-driven strath-terrace production assessed via dissimilar stream-process response to late Quaternary climate. Geomorphology 214, 223–244.CrossRefGoogle Scholar
Gilbert, G.K., 1877. Geology of the Henry Mountains. US Geological and Geographical Survey of the Rocky Mountain Region, Government Printing Office, Washington, D.C. https://doi.org/10.3133/70038096.CrossRefGoogle Scholar
Gran, K.B., Finnegan, N., Johnson, A.L., Belmont, P., Wittkop, C., Rittenour, T., 2013. Landscape evolution, valley excavation, and terrace development following abrupt postglacial base-level fall. Geological Society of America Bulletin 125, 1851–1864.CrossRefGoogle Scholar
Guérin, G., Christophe, C., Philippe, A., Murray, A.S., Thomsen, K.J., Tribolo, C., Urbanová, P., Jain, M., Guibert, P., Mercier, N., 2017. Absorbed dose, equivalent dose, measured dose rates, and implications for OSL age estimates: introducing the Average Dose Model. Quaternary Geochronology 41, 163–173.CrossRefGoogle Scholar
Guérin, G., Mercier, N., Adamiec, G., 2011. Dose-rate conversion factors: update. Ancient TL 29, 5–8.Google Scholar
Hack, J.T., 1960. Interpretation of erosional topography in humid temperate regions. American Journal of Science 258, 80–97.Google Scholar
Hancock, G.S., Anderson, R.S., 2002. Numerical modeling of fluvial strath-terrace formation in response to oscillating climate. Geological Society of America Bulletin 114, 1131–1142.2.0.CO;2>CrossRefGoogle Scholar
Harkins, N.W., Anastasio, D.J., Pazzaglia, F.J., 2005. Tectonic geomorphology of the Red Rock fault, insights into segmentation and landscape evolution of a developing range front normal fault. Journal of Structural Geology 27, 1925–1939.CrossRefGoogle Scholar
Howard, A.D., 1994. A detachment-limited model of drainage basin evolution. Water Resources Research 30, 2261–2285.CrossRefGoogle Scholar
Hudson, M.R., Paces, J.B., Turner, K.J., 2017. Tufa and water radiogenic geochemistry and tufa ages for two karst aquifers in the Buffalo National River region, northern Arkansas. In: Kuniansky, E.L., Spangler, L.E. (Eds.), US Geological Survey Karst Interest Group Proceedings, San Antonio, Texas, May 16–18, 2017. Scientific Investigations Report 2017-5023, 107–118.Google Scholar
Hudson, M.R., Turner, K.J., 2022. Late Paleozoic flexural extension and overprinting shortening in the southern Ozark dome, Arkansas, USA: evolving fault kinematics in the foreland of the Ouachita orogen. Tectonics 41, e2021TC006706. https://doi.org/10.1029/2021TC006706.CrossRefGoogle Scholar
Hudson, M.R., Turner, K.J., Bitting, C., 2011. Geology and karst landscapes of the Buffalo National River area, northern Arkansas. In: Kuniansky, E.L., U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26–29, 2011. U.S. Geological Survey Scientific Investigations Report 2011-5031, 191–212.Google Scholar
Hu, G., Zhang, J.-F., Qiu, W.-L., Zhou, L.-P., 2010. Residual OSL signals in modern fluvial sediments from the Yellow River (HuangHe) and the implications for dating young sediments. Quaternary Geochronology 5, 187–193.CrossRefGoogle Scholar
Jain, M., Murray, A.S., Botter-Jensen, L., 2004. Optically stimulated luminescence dating: how significant is incomplete light exposure in fluvial environments? Quaternaire 15, 143–157.CrossRefGoogle Scholar
Johnson, W.C., Willey, K.L., 2000. Isotopic and rock magnetic expression of environmental change at the Pleistocene–Holocene transition in the central Great Plains. Quaternary International 67, 89–106.CrossRefGoogle Scholar
Jones, R.A., Williams, J.W., Jackson, S.T., 2017. Vegetation history since the last glacial maximum in the Ozark highlands (USA): a new record from Cupola Pond, Missouri. Quaternary Science Reviews 170, 174–187.CrossRefGoogle Scholar
Keen-Zebert, A., Hudson, M.R., Shepherd, S.L., Thaler, E.A., 2017. The effect of lithology on valley width, terrace distribution, and bedload provenance in a tectonically stable catchment with flat-lying stratigraphy. Earth Surface Processes and Landforms 42, 1573–1587.CrossRefGoogle Scholar
King, J.E., 1973. Late Pleistocene palynology and biogeography of the Western Missouri Ozarks. Ecological Monographs 43, 539–565.CrossRefGoogle Scholar
Kirkby, M.J., 1986. A two dimensional simulation model for slope and stream evolution. In: Abrahams, A.D. (Ed.), Hillslope Processes, Binghamton Geomorphology Symposium 16. Allen and Unwin, Winchester, MA, pp. 203–222.Google Scholar
Lavé, J., Avouac, J.P., 2001. Fluvial incision and tectonic uplift across the Himalayas of central Nepal. Journal of Geophysical Research: Solid Earth 106, 26561–26591.CrossRefGoogle Scholar
Layzell, A.L., Mandel, R.D., Ludvigson, G.A., Rittenour, T.M., Smith, J.J., 2015. Forces driving Late Pleistocene (ca. 77–12 ka) landscape evolution in the Cimarron River valley, southwestern Kansas. Quaternary Research 84, 106–117.CrossRefGoogle Scholar
Limaye, A.B.S., Lamb, M.P., 2014. Numerical simulations of bedrock valley evolution by meandering rivers with variable bank material. Journal of Geophysical Research: Earth Surface 119, 927–950.CrossRefGoogle Scholar
Limaye, A.B.S., Lamb, M.P., 2016. Numerical model predictions of autogenic fluvial terraces and comparison to climate change expectations. Journal of Geophysical Research: Earth Surface 121, 512–544.CrossRefGoogle Scholar
Liritzis, I., Stamoulis, K., Papachristodoulou, C., Ioannides, K., 2013. A re-evaluation of radiation dose-rate conversion factors. Mediterranean Archaeology and Archaeometry 13(3), 1–15.Google Scholar
Lisiecki, L.E., Raymo, M.E., 2005. A Pliocene–Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20, PA1003. https://doi.org/10.1029/2004PA001071.Google Scholar
Marcotte, A.L., Neudorf, C.M., Langston, A.L., 2021. Lateral bedrock erosion and valley formation in a heterogeneously layered landscape, northeast Kansas. Earth Surface Processes and Landforms 46, 2248–2263.CrossRefGoogle Scholar
Marshall, J.A., Roering, J.J., Bartlein, P.J., Gavin, D.G., Granger, D.E., Rempel, A.W., Praskievicz, S.J., Hales, T.C., 2015. Frost for the trees: did climate increase erosion in unglaciated landscapes during the late Pleistocene? Science Advances 1, e1500715. https://doi.org/10.1126/sciadv.1500715.CrossRefGoogle ScholarPubMed
Marshall, J.A., Roering, J.J., Rempel, A.W., Shafer, S.L., Bartlein, P.J., 2021. Extensive frost weathering across unglaciated North America during the last glacial maximum. Geophysical Research Letters 48, e2020GL090305. https://doi.org/10.1029/2020GL090305.CrossRefGoogle Scholar
Meier, H.A., Nordt, L.C., Forman, S.L., Driese, S.G., 2013. Late Quaternary alluvial history of the middle Owl Creek drainage basin in central Texas: a record of geomorphic response to environmental change. Quaternary International 306, 24–41.CrossRefGoogle Scholar
Merritts, D.J., Vincent, K.R., Wohl, E.E., 1994. Long river profiles, tectonism, and eustasy: a guide to interpreting fluvial terraces. Journal of Geophysical Research: Solid Earth 99, 14031–14050.CrossRefGoogle Scholar
Montgomery, D.R., 2004. Observations on the role of lithology in strath terrace formation and bedrock channel width. American Journal of Science 304, 454–476.CrossRefGoogle Scholar
Mott, D., Luraas, J., 2004. Buffalo National River, Arkansas Water Resources Management Plan. National Park Service, U.S. Department of the Interior, Washington, DC, 144 pp.Google Scholar
Mudd, S.M., 2017. Detection of transience in eroding landscapes. Earth Surface Processes and Landforms 42, 24–41.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32, 57–73.CrossRefGoogle Scholar
Murray, A.S., Wintle, A.G., 2003. The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements 37, 377–381. https://doi.org/10.1016/S1350-4487(03)00053-2.CrossRefGoogle Scholar
Musgrove, M., Banner, J.L., Mack, L.E., Combs, D.M., James, E.W., Cheng, H., Edwards, R.L., 2001. Geochronology of Late Pleistocene to Holocene speleothems from central Texas: implications for regional paleoclimate. Geological Society of America Bulletin 113, 1532–1543.2.0.CO;2>CrossRefGoogle Scholar
Neely, B.L., 1985. The flood of December 1982 and the 100- and 500-year flood on the Buffalo River, Arkansas. US Geological Survey, Water-Resources Investigations Report 85–4192. https://doi.org/10.3133/wri854192.Google Scholar
Olley, J.M., Pietsch, T., Roberts, R.G., 2004. Optical dating of Holocene sediments from a variety of geomorphic settings using single grains of quartz. Geomorphology 60, 337–358.CrossRefGoogle Scholar
Olson, C., Nettleton, W., Porter, D., Brasher, B., 1997. Middle Holocene aeolian activity on the High Plains of west-central Kansas. The Holocene 7, 255–261.CrossRefGoogle Scholar
Otvos, E.G., 2013. Rapid and widespread response of the Lower Mississippi River to eustatic forcing during the last glacial-interglacial cycle: discussion. Geological Society of American Bulletin 125, 1369–1374.CrossRefGoogle Scholar
Paces, J.B., Hudson, M.R., Hudson, A.M., Turner, K.J., Bitting, C.J., Center, D., 2017. Isotopic Constraints on Middle Pleistocene Cave Evolution, Paleohydrologic Flow, and Environmental Conditions From Fitton Cave Speleothems, Buffalo National River, Arkansas. In: Kuniansky, E.L., Spangler, L.E. (Eds.), US Geological Survey Karst Interest Group Proceedings, San Antonio, Texas, May 16–18, 2017. Scientific Investigations Report 2017-5023, 119–132.Google Scholar
Pazzaglia, F.J., Brandon, M.T., 2001. A fluvial record of long-term steady-state uplift and erosion across the Cascadia forearc high, western Washington State. American Journal of Science 301, 385–431.CrossRefGoogle Scholar
Pederson, J.L., Anders, M.D., Rittenhour, T.M., Sharp, W.D., Gosse, J.C., Karlstrom, K.E., 2006. Using fill terraces to understand incision rates and evolution of the Colorado River in eastern Grand Canyon, Arizona. Journal of Geophysical Research: Earth Surface 111, F02003. https://doi.org/10.1029/2004JF000201.CrossRefGoogle Scholar
Personius, S.F., Kelsey, H.M., Grabau, P.C., 1993. Evidence for regional stream aggradation in the Central Oregon Coast Range during the Pleistocene-Holocene transition. Quaternary Research 40, 297–308.CrossRefGoogle Scholar
Porat, N., Duller, G., Roberts, H., Wintle, A., 2009. A simplified SAR protocol for TT-OSL. Radiation Measurements 44, 538–542.CrossRefGoogle Scholar
Prescott, J.R., Hutton, J.T., 1994. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements 23, 497–500.CrossRefGoogle Scholar
Rink, W.J., Odom, A.L., 1991. Natural alpha recoil particle radiation and ionizing radiation sensitivities in quartz detected with EPR: implications for geochronometry. International Journal of Radiation Applications and Instrumentation. Part D. Nuclear Tracks and Radiation Measurements 18, 163–173.CrossRefGoogle Scholar
Schanz, S.A., Montgomery, D.R., 2016. Lithologic controls on valley width and strath terrace formation. Geomorphology 258, 58–68.CrossRefGoogle Scholar
Schanz, S.A., Montgomery, D.R., Collins, B.D., Duvall, A.R., 2018. Multiple paths to straths: a review and reassessment of terrace genesis. Geomorphology 312, 12–23.CrossRefGoogle Scholar
Scheingross, J.S., Limaye, A.B., McCoy, S.W., Whittaker, A.C., 2020. The shaping of erosional landscapes by internal dynamics. Nature Reviews Earth & Environment 1, 661–676.CrossRefGoogle Scholar
Shen, Z., Mauz, B., Lang, A., 2011. Source-trap characterization of thermally transferred OSL in quartz. Journal of Physics D: Applied Physics 44, 295405. https://doi.org/10.1088/0022-3727/44/29/295405.CrossRefGoogle Scholar
Shen, Z., Tornqvist, T.E., Autin, W.J., Mateo, Z.R.P., Straub, K.M., Mauz, B., 2012. Rapid and widespread response of the Lower Mississippi River to eustatic forcing during the last glacial-interglacial cycle. Geological Society of America Bulletin 124, 690–704.CrossRefGoogle Scholar
Sionneau, T., Bout-Roumazeilles, V., Meunier, G., Kissel, C., Flower, B.P., Bory, A., Tribovillard, N., 2013. Atmospheric re-organization during Marine Isotope Stage 3 over the North American continent: sedimentological and mineralogical evidence from the Gulf of Mexico. Quaternary Science Reviews 81, 62–73.CrossRefGoogle Scholar
Spratt, R.M., Lisiecki, L.E., 2016. A Late Pleistocene sea level stack. Climate of the Past 12, 1079–1092.CrossRefGoogle Scholar
Thiel, C., Buylaert, J.-P., Murray, A.S., Elmejdoub, N., Jedoui, Y., 2012. A comparison of TT-OSL and post-IR IRSL dating of coastal deposits on Cap Bon peninsula, north-eastern Tunisia. Quaternary Geochronology 10, 209–217.CrossRefGoogle Scholar
Turner, K.J., Hudson, M.R., 2010. Geologic map of the Maumee quadrangle, Marion and Searcy Counties, Arkansas. U.S. Geological Survey Scientific Investigations Map 3134, 1:24,000 scale.CrossRefGoogle Scholar
Van Der Woerd, J., Xu, X., Li, H., Tapponnier, P., Meyer, B., Ryerson, F.J., Meriaux, A.-S., Xu, Z., 2001. Rapid active thrusting along the northwestern range front of the Tanghe Nan Shan (western Gansu, China). Journal of Geophysical Research: Solid Earth 106, 30475–30504.CrossRefGoogle Scholar
Wang, X., Lu, Y., Wintle, A., 2006. Recuperated OSL dating of fine-grained quartz in Chinese loess. Quaternary Geochronology 1, 89–100.CrossRefGoogle Scholar
Waters, M.R., Nordt, L.C., 1995. Late Quaternary floodplain history of the Brazos River in east-central Texas. Quaternary Research 43, 311–319.CrossRefGoogle Scholar
Wegmann, K.W., Pazzaglia, F.J., 2002. Holocene strath terraces, climate change, and active tectonics: the Clearwater River basin, Olympic Peninsula, Washington State. Geological Society of America Bulletin 114, 731–744.2.0.CO;2>CrossRefGoogle Scholar
Wegmann, K.W., Pazzaglia, F.J., 2009. Late Quaternary fluvial terraces of the Romagna and Marche Apennines, Italy: climatic, lithologic, and tectonic controls on terrace genesis in an active orogen. Quaternary Science Reviews 28, 137–165. https://doi.org/10.1016/j.quascirev.2008.10.006.CrossRefGoogle Scholar
Whipple, K.X., Tucker, G.E., 1999. Dynamics of the stream-power river incision model: implications for height limits of mountain ranges, landscape response timescales, and research needs. Journal of Geophysical Research: Solid Earth 104, 17661–17674.CrossRefGoogle Scholar
Wintle, A.G., Murray, A.S., 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41, 369–391.CrossRefGoogle Scholar
Wong, C.I., Banner, J.L., Musgrove, M., 2015. Holocene climate variability in Texas, USA: an integration of existing paleoclimate data and modeling with a new, high-resolution speleothem record. Quaternary Science Reviews 127, 155–173.CrossRefGoogle Scholar
Zunka, J.P.P., 2018. Controls on Process and Form in Alluvial and Bedrock Meandering Rivers. PhD dissertation, Oregon State University, Corvallis, OR.Google Scholar
Supplementary material: File

Rodrigues et al. supplementary material

Rodrigues et al. supplementary material

Download Rodrigues et al. supplementary material(File)
File 74 KB