| Eocene and Oligocene paleosols of central Oregon GJ Retallack, EA Bestland, TJ Fremd Geological Society of America, 1999 | 182 | 1999 |
| Variation in performance of surfactant loading and resulting nitrate removal among four selected natural zeolites H Guan, E Bestland, C Zhu, H Zhu, D Albertsdottir, J Hutson, CT Simmons, ... Journal of hazardous materials 183 (1-3), 616-621, 2010 | 164 | 2010 |
| Fossil soils and grasses of a middle Miocene East African grassland GJ Retallack, DP Dugas, EA Bestland Science 247 (4948), 1325-1328, 1990 | 154 | 1990 |
| Fractured bedrock and saprolite hydrogeologic controls on groundwater/surface-water interaction: a conceptual model (Australia) EW Banks, CT Simmons, AJ Love, R Cranswick, AD Werner, EA Bestland, ... Hydrogeology Journal 8 (17), 1969-1989, 2009 | 145 | 2009 |
| Laboratory assessment of factors affecting soil clogging of soil aquifer treatment systems P Pavelic, PJ Dillon, M Mucha, T Nakai, KE Barry, E Bestland Water research 45 (10), 3153-3163, 2011 | 139 | 2011 |
| Soil organic matter decomposition and turnover in a tropical Ultisol: evidence from δ13C, δ15N and geochemistry ES Krull, EA Bestland, WP Gates Radiocarbon 44 (1), 93-112, 2002 | 112 | 2002 |
| Age and origin of Terra Rossa soils in the Coonawarra area of South Australia AC Mee, EA Bestland, NA Spooner Geomorphology 58 (1-4), 1-25, 2004 | 70 | 2004 |
| Stepwise climate change recorded in Eocene-Oligocene paleosol sequences from central Oregon EA Bestland, GJ Retallack, CC Swisher, Iii The Journal of Geology 105 (2), 153-172, 1997 | 67 | 1997 |
| Geologic framework of the Clarno Unit, John Day Fossil Beds National Monument, central Oregon EA Bestland, PE Hammond, DLS Blackwell, MA Kays, GJ Retallack, ... Oregon Geology 61 (1), 3-19, 1999 | 63 | 1999 |
| Late Eocene detrital laterites in central Oregon: Mass balance geochemistry, depositional setting, and landscape evolution EA Bestland, GJ Retallack, AE Rice, A Mindszenty Geological Society of America Bulletin 108 (3), 285-302, 1996 | 62 | 1996 |
| Miocene paleosols and habitats of Proconsul on Rusinga Island, Kenya GJ Retallack, EA Bestland, DP Dugas Journal of Human Evolution 29 (1), 53-91, 1995 | 55 | 1995 |
| Characterization of dissolved organic matter for prediction of trihalomethane formation potential in surface and sub-surface waters J Awad, J van Leeuwen, C Chow, M Drikas, RJ Smernik, ... Journal of hazardous materials 308, 430-439, 2016 | 48 | 2016 |
| Distinguishing sources of base cations in irrigated and natural soils: evidence from strontium isotopes GP Green, EA Bestland, GS Walker Biogeochemistry 68, 199-225, 2004 | 48 | 2004 |
| Alluvial terraces and paleosols as indicators of early Oligocene climate change (John Day Formation, Oregon) EA Bestland Journal of Sedimentary Research 67 (5), 840-855, 1997 | 45 | 1997 |
| Stratigraphy, paleopedology, and geochemistry of the middle Miocene Mascall Formation (type area, central Oregon, USA) EA Bestland, MS Forbes, ES Krull, GJ Retallack, T Fremd PaleoBios 28 (2), 41-61, 2008 | 37 | 2008 |
| Palaeoenvironments of Early Miocene Kisingiri volcano Proconsul sites: evidence from carbon isotopes, palaeosols and hydromagmatic deposits EA Bestland, ES Krull Journal of the Geological Society 156 (5), 965-976, 1999 | 37 | 1999 |
| Origin of the sedimentary deposits of the Naracoorte Caves, South Australia MS Forbes, EA Bestland Geomorphology 86 (3-4), 369-392, 2007 | 36 | 2007 |
| Geochemistry (δ13C, δ15N, 13C NMR) and residence times (14C and OSL) of soil organic matter from red-brown earths of South Australia: Implications for soil genesis ES Krull, EA Bestland, JO Skjemstad, JF Parr Geoderma 132 (3-4), 344-360, 2006 | 36 | 2006 |
| John Day Basin Paleontology: Field Trip Guide and Road Log, 1994 Society of Vertebrate Paleontology Annual Meeting TJ Fremd, EA Bestland, GJ Retallack Northwest Interpretive Association, 1997 | 36 | 1997 |
| Weathering flux and CO2 consumption determined from palaeosol sequences across the Eocene–Oligocene transition EA Bestland Palaeogeography, Palaeoclimatology, Palaeoecology 156 (3-4), 301-326, 2000 | 33 | 2000 |
