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SOIL DEVELOPMENT ON MODERN DISTRIBUTIVE FLUVIAL SYSTEMS: PRELIMINARY OBSERVATIONS WITH IMPLICATIONS FOR INTERPRETATION OF PALEOSOLS IN THE ROCK RECORD ADRIAN J. HARTLEY Department of Geology and Petroleum Geology, School of Geosciences, University of Aberdeen, Aberdeen, AB24 3UE, UK e-mail: a.hartley@abdn.ac.uk GARY S. WEISSMANN AND PROMA BHATTACHARAYYA Department of Earth and Planetary Sciences, University of New Mexico, MSC03 2040, 1 University of New Mexico, Albuquerque, New Mexico 87131-0001, USA GARY J. NICHOLS Department of Earth Sciences, Royal Holloway, University of London, Egham, Surrey, TW20 0EX, UK LOUIS A. SCUDERI Department of Earth and Planetary Sciences, University of New Mexico, MSC03 2040, 1 University of New Mexico, Albuquerque, New Mexico 87131-0001, USA STEPHANIE K. DAVIDSON AND SOPHIE LELEU* Department of Geology and Petroleum Geology, School of Geosciences, University of Aberdeen, Aberdeen, AB24 3UE, UK *Present address: EA4592 G&E, ENSEGID, Institut Polytechnique de Bordeaux, 1 allée Daguin, 33 607 Pessac, France TAPAN CHAKRABORTY AND PARTHASARATHI GHOSH Indian Statistical Institute, 205 B.T. Road, Kolkata, India AND ANNE E. MATHER School of Geography, Earth and Environmental Sciences, Plymouth University, Drake Circus, Plymouth, PL4 8AA, UK ABSTRACT: Understanding of controls on the distribution of soils in modern sedimentary basins facilitates interpretation of paleosols in the rock record. Here, we present information on soil distribution from a number of modern distributive fluvial systems (DFSs) in sedimentary basins developed in different climatic and tectonic settings. DFSs form an important part of modern alluvial sedimentary basins, and an understanding of the controls on soil development in these settings should facilitate interpretation of the alluvial rock record. The studied areas include: the Pilcomayo and Bermejo DFSs in the Andean foreland of Argentina, the Tista DFS of the Himalayan foreland basin in northern India, and the Okavango DFS developed in an intracontinental rift basin in Botswana. Soils in each of the examples are relatively immature and weakly developed. Where present, downdip changes (over distances >100 km) from relatively well-drained, relatively dry soils in sandy proximal areas to more poorly drained, relatively wet soils in more distal, clay-rich areas can be recognized. In the Andean example, this change
is considered to be related to a downdip increase in precipitation and decreasing depth to water table. In the Himalayan system, this is considered to be due to a combination of decreasing depth to water table and increased surface flooding due to direct, monsoon-driven precipitation on the DFS surface. An increase in poorly drained soil development occurs near the toe of the DFS in Botswana, despite high transmission losses across the system. A key implication from these modern systems is that a change from well-drained to poorly drained soils is controlled by hydrology. This change occurs along a single isochronous surface that may extend for hundreds of kilometers and could be preserved in the rock record. Rock record examples that describe a downdip change from well-drained to poorly drained soils have been documented previously and are attributed to tectonic, climatic, autocyclic, and hydromorphic controls. Our studies from modern DFSs would suggest that a hydromorphic control is likely to be the most important factor. Criteria derived from modern DFSs for distinguishing between changes in soil type that record climate change include the observation that paleosols developed in the proximal well-drained area are likely to be associated with a sandy parent material and sand-dominated channel facies. In contrast, in the distal DFSs, more poorly drained soils are likely to be developed on a silt- or clay-rich parent material interbedded with a mixture of sandy and muddy meandering channel-fill deposits, crevasse splays, and floodplain sands and muds. Paleosols that record climate change should show no discernible relationship between parent material and soil type. While similar relationships between soil type and parent material have been described previously, their distribution within the context of a DFS has not been widely documented.
Page 2 and 3: New Frontiers in Paleopedology and
Page 4 and 5: A SHORT HISTORY AND LONG FUTURE FOR
Page 6 and 7: CO 2 CONCENTRATIONS IN VERTISOLS: S
Page 8 and 9: SOIL AND LANDSCAPE MEMORY OF CLIMAT
Page 10 and 11: PALEOCLIMATIC APPLICATIONS AND MODE
Page 12 and 13: ALLUVIAL STACKING PATTERN ANALYSIS
Page 14 and 15: PROGRADING DISTRIBUTIVE FLUVIAL SYS
Page 18 and 19: A PEDOSTRATIGRAPHIC APPROACH TO NON
Page 20 and 21: oth higher temperatures and an inte
Page 22: EARLY CAMBRIAN HUMID, TROPICAL, COA

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