Science Journals

Total Page:16

File Type:pdf, Size:1020Kb

Science Journals Early human impacts and ecosystem reorganization in southern-central Africa Item Type Article; text Authors Thompson, J.C.; Wright, D.K.; Ivory, S.J.; Choi, J.-H.; Nightingale, S.; Mackay, A.; Schilt, F.; Otárola-Castillo, E.; Mercader, J.; Forman, S.L.; Pietsch, T.; Cohen, A.S.; Arrowsmith, J.R.; Welling, M.; Davis, J.; Schiery, B.; Kaliba, P.; Malijani, O.; Blome, M.W.; O'Driscoll, C.A.; Mentzer, S.M.; Miller, C.; Heo, S.; Choi, J.; Tembo, J.; Mapemba, F.; Simengwa, D.; Gomani-Chindebvu, E. Citation Thompson, J. C., Wright, D. K., Ivory, S. J., Choi, J.-H., Nightingale, S., Mackay, A., Schilt, F., Otárola-Castillo, E., Mercader, J., Forman, S. L., Pietsch, T., Cohen, A. S., Arrowsmith, J. R., Welling, M., Davis, J., Schiery, B., Kaliba, P., Malijani, O., Blome, M. W., … Gomani-Chindebvu, E. (2021). Early human impacts and ecosystem reorganization in southern-central Africa. Science Advances, 7(19). DOI 10.1126/sciadv.abf9776 Publisher American Association for the Advancement of Science Journal Science Advances Rights Copyright © 2021 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S.Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC). Download date 01/10/2021 20:13:45 Item License https://creativecommons.org/licenses/by-nc/4.0/ Version Final published version Link to Item http://hdl.handle.net/10150/660624 SCIENCE ADVANCES | RESEARCH ARTICLE ANTHROPOLOGY Copyright © 2021 The Authors, some rights reserved; Early human impacts and ecosystem reorganization exclusive licensee American Association in southern-central Africa for the Advancement Jessica C. Thompson1,2*†, David K. Wright3,4*†, Sarah J. Ivory5*†, Jeong-Heon Choi6, Sheila Nightingale7, of Science. No claim to 8 9,10 11 12,13,14 15 original U.S. Government Alex Mackay , Flora Schilt , Erik Otárola-Castillo , Julio Mercader , Steven L. Forman , Works. Distributed 16 17 18 19,20 21 Timothy Pietsch , Andrew S. Cohen , J. Ramón Arrowsmith , Menno Welling , Jacob Davis , under a Creative 22 23 23 24 8 Benjamin Schiery , Potiphar Kaliba , Oris Malijani , Margaret W. Blome , Corey A. O’Driscoll , Commons Attribution Susan M. Mentzer9,25, Christopher Miller9,26, Seoyoung Heo6, Jungyu Choi27, Joseph Tembo23, NonCommercial Fredrick Mapemba23, Davie Simengwa28, Elizabeth Gomani-Chindebvu29 License 4.0 (CC BY-NC). Modern Homo sapiens engage in substantial ecosystem modification, but it is difficult to detect the origins or early consequences of these behaviors. Archaeological, geochronological, geomorphological, and paleoenviron- mental data from northern Malawi document a changing relationship between forager presence, ecosystem organization, and alluvial fan formation in the Late Pleistocene. Dense concentrations of Middle Stone Age artifacts and alluvial fan systems formed after ca. 92 thousand years ago, within a paleoecological context with no analog Downloaded from in the preceding half-million-year record. Archaeological data and principal coordinates analysis indicate that early anthropogenic fire relaxed seasonal constraints on ignitions, influencing vegetation composition and erosion. This operated in tandem with climate-driven changes in precipitation to culminate in an ecological transition to an early, pre-agricultural anthropogenic landscape. http://advances.sciencemag.org/ INTRODUCTION interactions between foragers and their environments that suggest Modern humans act as powerful agents of ecosystem transformation. that these behaviors were fundamental to the evolution of our spe- They have extensively and intentionally modified their environments cies (2–4). Fossil and genetic data indicate that Homo sapiens were for tens of millennia, leading to much debate about when and how the present in Africa by ~315 thousand years (ka) ago, and archaeolog- first human-dominated ecosystems arose (1). A growing body of ar- ical data show notable increases in the complexity of behavior that chaeological and ethnographic evidence shows substantial, recursive took place across the continent within the past ~300- to 200-ka span at the end of the Middle Pleistocene (Chibanian) (5). Since our emer- gence as a species, humans have come to rely on technological in- 1 2 Department of Anthropology, Yale University, New Haven, CT, USA. Institute of Hu- novation, seasonal scheduling, and complex social cooperation to man Origins, P.O. Box 874101, Tempe, AZ 85287, USA. 3Department of Archaeology, Conservation and History, University of Oslo, Oslo, Norway. 4State Key Laboratory of thrive. These attributes have enabled us to exploit previously un- on July 16, 2021 Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of inhabited or extreme environments and resources, so that today hu- Sciences, Xian, China. 5Department of Geosciences and Earth and Environmental Sys- mans are the only pan-global animal species (6). Fire has played a key tems Institute, Pennsylvania State University, University Park, PA, USA. 6Depart- ment of Earth and Environmental Sciences, Korea Basic Science Institute, Ochang, role in this transformation (7). Republic of Korea. 7Department of Anthropology, City University of New York, Biological models suggest that adaptations for cooked food Graduate Center, New York, NY, USA. 8Centre for Archaeological Science, School of extend back at least 2 million years, but regular archaeological evi- Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW, dence for controlled use of fire does not appear until the end of the Australia. 9Institute for Archaeological Sciences and Senckenberg Centre for Human Evolution and Palaeoenvironment, University of Tübingen, Tübingen, Germany. Middle Pleistocene (8). A marine core with a dust record drawn 10Universidade do Algarve, Interdisciplinary Center for Archaeology and Evolution of from a wide swath of the African continent shows that over the past Human Behavior (ICArEHB), FCHS, Campus Gambelas, J27, Faro 8005-139, Portugal. million years, peaks in elemental carbon occurred after ~400 ka, 11Department of Anthropology, Purdue University, West Lafayette, IN, USA. 12Depart- ment of Anthropology and Archaeology, University of Calgary, Calgary, AB, Canada. predominately during shifts from interglacial to glacial conditions, 13Max Planck Institute for the Science of Human History, Jena, Germany. 14Institut but also during the Holocene (9). This suggests that fire was less Català de Paleoecologia Humana i Evolució Social (IPHES), Zona Educacional, 4– common in sub-Saharan Africa before ~400 ka and that by the Campus Sescelades URV (Edifici W3), 43007 Tarragona, Spain. 15Department of 16 Holocene, there was a substantial anthropogenic contribution (9). Geosciences, Baylor University, Waco, TX, USA. Australian Rivers Institute, Griffith University, Brisbane, QLD, Australia. 17Department of Geosciences, University of Fire is a tool that has been used by pastoralists to open and maintain Arizona, Tucson, AZ, USA. 18School of Earth and Space Exploration, Arizona State grasslands throughout the Holocene (10). However, detecting the 19 University, Tempe, AZ, USA. Reinwardt Academy, Amsterdam University of the Arts, contexts and ecological impacts of fire use by Pleistocene early Amsterdam, Netherlands. 20African Heritage Ltd., Box 622, Zomba, Malawi. 21Inde- pendent Researcher, New Haven, CT, USA. 22Biostatistics Department, Medpace hunter-gatherers is more complex (11). Inc., Cincinnati, OH, USA. 23Malawi Department of Museums and Monuments, Lilongwe, Fire is known both ethnographically and archaeologically as an Malawi. 24Department of Geological Sciences, East Carolina University, Greenville, NC, engineering tool for resource manipulation, including improvement USA. 25School of Anthropology, University of Arizona, Tucson, AZ, USA. 26SFF Cen- tre for Early Sapiens Behaviour (SapienCE), University of Bergen, Bergen, Norway. of subsistence returns or modification of raw materials, with these 27Gyeongju National Research Institute of Cultural Heritage, Gyeongju, Republic of activities often associated with communal planning and requiring sub- Korea. 28Lanujos Social Research and Consultancy, Blantyre, Malawi. 29Ministry of stantial ecological knowledge (2, 12, 13). Landscape-scale fires allow Civic Education and National Unity, Lilongwe, Malawi. hunter-gatherers to drive game, control pests, and enhance produc- *Corresponding author. Email: [email protected] (J.C.T); david.wright@ iakh.uio.no (D.K.W.); [email protected] (S.J.I.) tivity of habitat (2). On-site fire facilitates cooking, warmth, preda- †These authors contributed equally to this work. tor defense, and social cohesion (14). However, there is substantial Thompson et al., Sci. Adv. 2021; 7 : eabf9776 5 May 2021 1 of 13 SCIENCE ADVANCES | RESEARCH ARTICLE ambiguity regarding the extent to which fires by hunter-gatherers can regional relief and piedmont slopes over an extended time, fault reconfigure components of a landscape, such as ecological commu- activity in this region likely slowed since the Middle Pleistocene nity structure and geomorphology (15, 16). (20). After ~800 ka until shortly after 100 ka, the hydrology of Understanding the development of human-induced ecological Lake Malawi became primarily climate driven (21). Therefore, change is problematic without well-dated archaeological and geo- neither is likely the sole explanation for Late Pleistocene alluvial fan morphic data from multiple
Recommended publications
  • Climatic Events During the Late Pleistocene and Holocene in the Upper Parana River: Correlation with NE Argentina and South-Central Brazil Joseh C
    Quaternary International 72 (2000) 73}85 Climatic events during the Late Pleistocene and Holocene in the Upper Parana River: Correlation with NE Argentina and South-Central Brazil JoseH C. Stevaux* Universidade Federal do Rio Grande do Sul - Instituto de GeocieL ncias - CECO, Universidade Estadual de Maringa& - Geography Department, 87020-900 Maringa& ,PR} Brazil Abstract Most Quaternary studies in Brazil are restricted to the Atlantic Coast and are mainly based on coastal morphology and sea level changes, whereas research on inland areas is largely unexplored. The study area lies along the ParanaH River, state of ParanaH , Brazil, at 223 43S latitude and 533 10W longitude, where the river is as yet undammed. Paleoclimatological data were obtained from 10 vibro cores and 15 motor auger holes. Sedimentological and pollen analyses plus TL and C dating were used to establish the following evolutionary history of Late Pleistocene and Holocene climates: First drier episode ?40,000}8000 BP First wetter episode 8000}3500 BP Second drier episode 3500}1500 BP Second (present) wet episode 1500 BP}Present Climatic intervals are in agreement with prior studies made in southern Brazil and in northeastern Argentina. ( 2000 Elsevier Science Ltd and INQUA. All rights reserved. 1. Introduction the excavation of Sete Quedas Falls on the ParanaH River (today the site of the Itaipu dam). Barthelness (1960, Geomorphological and paleoclimatological studies of 1961) de"ned a regional surface in the Guaira area de- the Upper ParanaH River Basin are scarce and regional in veloped at the end of the Pleistocene (Guaira Surface) nature. King (1956, pp. 157}159) de"ned "ve geomor- and correlated it with the Velhas Cycle.
    [Show full text]
  • Sea Level and Global Ice Volumes from the Last Glacial Maximum to the Holocene
    Sea level and global ice volumes from the Last Glacial Maximum to the Holocene Kurt Lambecka,b,1, Hélène Roubya,b, Anthony Purcella, Yiying Sunc, and Malcolm Sambridgea aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; bLaboratoire de Géologie de l’École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and cDepartment of Earth Sciences, University of Hong Kong, Hong Kong, China This contribution is part of the special series of Inaugural Articles by members of the National Academy of Sciences elected in 2009. Contributed by Kurt Lambeck, September 12, 2014 (sent for review July 1, 2014; reviewed by Edouard Bard, Jerry X. Mitrovica, and Peter U. Clark) The major cause of sea-level change during ice ages is the exchange for the Holocene for which the direct measures of past sea level are of water between ice and ocean and the planet’s dynamic response relatively abundant, for example, exhibit differences both in phase to the changing surface load. Inversion of ∼1,000 observations for and in noise characteristics between the two data [compare, for the past 35,000 y from localities far from former ice margins has example, the Holocene parts of oxygen isotope records from the provided new constraints on the fluctuation of ice volume in this Pacific (9) and from two Red Sea cores (10)]. interval. Key results are: (i) a rapid final fall in global sea level of Past sea level is measured with respect to its present position ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y and contains information on both land movement and changes in before present (30 ka BP); (ii) a slow fall to −134 m from 29 to 21 ka ocean volume.
    [Show full text]
  • The Easternmost Occurrence of Mammut Pacificus (Proboscidea: Mammutidae), Based on a Partial Skull from Eastern Montana, USA
    The easternmost occurrence of Mammut pacificus (Proboscidea: Mammutidae), based on a partial skull from eastern Montana, USA Andrew T. McDonald1, Amy L. Atwater2, Alton C. Dooley Jr1 and Charlotte J.H. Hohman2,3 1 Western Science Center, Hemet, CA, United States of America 2 Museum of the Rockies, Montana State University, Bozeman, MT, United States of America 3 Department of Earth Sciences, Montana State University, Bozeman, MT, United States of America ABSTRACT Mammut pacificus is a recently described species of mastodon from the Pleistocene of California and Idaho. We report the easternmost occurrence of this taxon based upon the palate with right and left M3 of an adult male from the Irvingtonian of eastern Montana. The undamaged right M3 exhibits the extreme narrowness that characterizes M. pacificus rather than M. americanum. The Montana specimen dates to an interglacial interval between pre-Illinoian and Illinoian glaciation, perhaps indicating that M. pacificus was extirpated in the region due to habitat shifts associated with glacial encroachment. Subjects Biogeography, Evolutionary Studies, Paleontology, Zoology Keywords Mammut pacificus, Mammutidae, Montana, Irvingtonian, Pleistocene INTRODUCTION Submitted 7 May 2020 The recent recognition of the Pacific mastodon (Mammut pacificus (Dooley Jr et al., 2019)) Accepted 3 September 2020 as a new species distinct from and contemporaneous with the American mastodon Published 16 November 2020 (M. americanum) revealed an unrealized complexity in North American mammutid Corresponding author evolution during the Pleistocene. Dooley Jr et al. (2019) distinguished M. pacificus from Andrew T. McDonald, [email protected] M. americanum by a suite of dental and skeletal features: (1) upper third molars (M3) Academic editor and lower third molars (m3) much narrower relative to length in M.
    [Show full text]
  • Variable Impact of Late-Quaternary Megafaunal Extinction in Causing
    Variable impact of late-Quaternary megafaunal SPECIAL FEATURE extinction in causing ecological state shifts in North and South America Anthony D. Barnoskya,b,c,1, Emily L. Lindseya,b, Natalia A. Villavicencioa,b, Enrique Bostelmannd,2, Elizabeth A. Hadlye, James Wanketf, and Charles R. Marshalla,b aDepartment of Integrative Biology, University of California, Berkeley, CA 94720; bMuseum of Paleontology, University of California, Berkeley, CA 94720; cMuseum of Vertebrate Zoology, University of California, Berkeley, CA 94720; dRed Paleontológica U-Chile, Laboratoria de Ontogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Chile; eDepartment of Biology, Stanford University, Stanford, CA 94305; and fDepartment of Geography, California State University, Sacramento, CA 95819 Edited by John W. Terborgh, Duke University, Durham, NC, and approved August 5, 2015 (received for review March 16, 2015) Loss of megafauna, an aspect of defaunation, can precipitate many megafauna loss, and if so, what does this loss imply for the future ecological changes over short time scales. We examine whether of ecosystems at risk for losing their megafauna today? megafauna loss can also explain features of lasting ecological state shifts that occurred as the Pleistocene gave way to the Holocene. We Approach compare ecological impacts of late-Quaternary megafauna extinction The late-Quaternary impact of losing 70–80% of the megafauna in five American regions: southwestern Patagonia, the Pampas, genera in the Americas (19) would be expected to trigger biotic northeastern United States, northwestern United States, and Berin- transitions that would be recognizable in the fossil record in at gia. We find that major ecological state shifts were consistent with least two respects.
    [Show full text]
  • A Possible Late Pleistocene Impact Crater in Central North America and Its Relation to the Younger Dryas Stadial
    A POSSIBLE LATE PLEISTOCENE IMPACT CRATER IN CENTRAL NORTH AMERICA AND ITS RELATION TO THE YOUNGER DRYAS STADIAL SUBMITTED TO THE FACULTY OF THE UNIVERSITY OF MINNESOTA BY David Tovar Rodriguez IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE Howard Mooers, Advisor August 2020 2020 David Tovar All Rights Reserved ACKNOWLEDGEMENTS I would like to thank my advisor Dr. Howard Mooers for his permanent support, my family, and my friends. i Abstract The causes that started the Younger Dryas (YD) event remain hotly debated. Studies indicate that the drainage of Lake Agassiz into the North Atlantic Ocean and south through the Mississippi River caused a considerable change in oceanic thermal currents, thus producing a decrease in global temperature. Other studies indicate that perhaps the impact of an extraterrestrial body (asteroid fragment) could have impacted the Earth 12.9 ky BP ago, triggering a series of events that caused global temperature drop. The presence of high concentrations of iridium, charcoal, fullerenes, and molten glass, considered by-products of extraterrestrial impacts, have been reported in sediments of the same age; however, there is no impact structure identified so far. In this work, the Roseau structure's geomorphological features are analyzed in detail to determine if impacted layers with plastic deformation located between hard rocks and a thin layer of water might explain the particular shape of the studied structure. Geophysical data of the study area do not show gravimetric anomalies related to a possible impact structure. One hypothesis developed on this works is related to the structure's shape might be explained by atmospheric explosions dynamics due to the disintegration of material when it comes into contact with the atmosphere.
    [Show full text]
  • Overkill, Glacial History, and the Extinction of North America's Ice Age Megafauna
    PERSPECTIVE Overkill, glacial history, and the extinction of North America’s Ice Age megafauna PERSPECTIVE David J. Meltzera,1 Edited by Richard G. Klein, Stanford University, Stanford, CA, and approved September 23, 2020 (received for review July 21, 2020) The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial−interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that pre- vious glacial−interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species’ histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene−Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial−interglacial transitions and the very last one was a human presence.
    [Show full text]
  • ARCL 0141 Mediterranean Prehistory
    INSTITUTE OF ARCHAEOLOGY ARCL 0141 Mediterranean Prehistory 2019-20, Term 1 - 15 CREDITS Deadlines for coursework: 11th November 2019, 13th January 2020 Coordinator: Dr. Borja Legarra Herrero [email protected] Office 106, tel. (0) 20 7679 1539 Please see the last page of this document for important information about submission and marking procedures, or links to the relevant webpages 1 OVERVIEW Introduction This course reunites the study and analysis of prehistoric societies around the Mediterranean basin into a coherent if diverse exploration. It takes a long-term perspective, ranging from the first modern human occupation in the region to the start of the 1st millennium BCE, and a broad spatial approach, searching for the overall trends and conditions that underlie local phenomena. Opening topics include the glacial Mediterranean and origins of seafaring, early Holocene Levantine-European farming, and Chalcolithic societies. The main body of the course is formed by the multiple transformations of the late 4th, 3rd and 2nd millennium BC, including the environmental ‘mediterraneanisation’ of the basin, the rise of the first complex societies in east and west Mediterranean and the formation of world-system relations at the east Mediterranean. A final session examines the transition to the Iron Age in the context of the emergence of pan-Mediterranean networks, and this also acts as a link to G202. This course is designed to interlock with G206, which explores Mediterranean dynamics from a diachronic and comparative perspective. Equally, it can be taken in conjunction with courses in the prehistory of specific regions, such as the Aegean, Italy, the Levant, Anatolia and Egypt, as well as Europe and Africa.
    [Show full text]
  • Pleistocene - the Ice Ages
    Pleistocene - the Ice Ages Sleeping Bear Dunes National Lakeshore Pleistocene - the Ice Ages • Stage is now set to understand the nature of flora and vegetation of North America and Great Lakes • Pliocene (end of Tertiary) - most genera had already originated (in palynofloras) • Flora was in place • Vegetation units (biomes) already derived Pleistocene - the Ice Ages • In the Pleistocene, earth experienced intensification towards climatic cooling • Culminated with a series of glacial- interglacial cycles • North American flora and vegetation profoundly influenced by these “ice-age” events Pleistocene - the Ice Ages What happened in the Pleistocene? 18K ya • Holocene (Recent) - the present interglacial started ~10,000 ya • Wisconsin - the last glacial (Würm in Europe) occurred between 115,000 ya - 10,000 ya • Height of Wisconsin glacial activity (most intense) was 18,000 ya - most intense towards the end of the glacial period Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal plains become extensive • continental islands disappeared and land bridges exposed 100 m line Beringia Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal plains become extensive • continental islands disappeared and land bridges exposed Malaysia to Asia & New Guinea and New Caledonia to Australia Present Level 100 m Level Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal
    [Show full text]
  • Late Pleistocene Geochronology of European Russia
    [RADIOCARBON, VOL. 35, No. 3, 1993, P. 421-427] LATE PLEISTOCENE GEOCHRONOLOGY OF EUROPEAN RUSSIA KU. A. ARSLANOV Geographical Research Institute, St. Petersburg State University, St. Petersburg 199004 Russia 14C ABSTRACT. I constructed a Late Pleistocene geochronological scale for European Russia employing dating and paleo- botanical studies of several reference sections. MIKULIN0 (RISS-WURM) INTERGLACIAL AND EARLY VALDAI (EARLY WURM) STAGES AND INTERSTADIALS 230Th/ I employed a modified 4U dating method (Arslanov et al. 1976, 1978, 1981) to determine shell ages. I learned that 232Th is present only in the outer layer of shells; thus, it is not necessary to correct for 230Th if the surface (-30% by weight) is removed. A great many shells were parallel- dated by 14C and 23°Th/234U methods; results corresponded well for young shells (to 13-14 ka). Older shells appear to be younger due to recent carbonate contamination. Shells from transgression sediments of the Barents, White and Black Seas were chosen as most suitable for dating, based on appearance. Table 1 presents measured ages for these shells. The data show that the inner fractions of shells sampled from Boreal (Eem) transgression deposits of the Barents and White Seas date to 86-114 ka. Shells from sediments of the Black Sea Karangat transgression, which correlates to the Boreal, date to 95-115 ka. 23°Th/234U dating of shells and coral show that shells have younger ages than corals; this appears to result from later uranium penetration into shells (Arslanov et a1.1976). Boreal transgression sediments on the Kola peninsula can be placed in the Mikulino interglacial based on shell, microfauna, diatom and pollen studies (Arslanov et at.
    [Show full text]
  • A Reexamination of Late-Pleistocene Boreal Forest Reconstructions for the Southern High Plains
    QUATERNARY RESEARCH 28,238-244 (1987) A Reexamination of Late-Pleistocene Boreal Forest Reconstructions for the Southern High Plains VANCE T. HOLLIDAY Department of Geography, Science Hall, University of Wisconsin, Madison, Wisconsin 53706 Received March 9, 1987 Previous paleoecological research on the Southern High Plains resulted in development of a late Quatemary chronology of “pollen-analytical episodes” and the proposal that boreal forest existed in the region in the late Pleistocene. These interpretations are now considered untenable because (1) a number of the radiocarbon ages are questionable, (2) there are serious problems of differential pollen preservation and reproducibility of the pollen data, (3) there is an absence of supporting geological or paleontological data, and (4) the soils of the area contain none of the distinctive pedologicd characteristics produced by a boreal forest. Available data suggest that the region was primarily an open grassland or grassland with some nonconiferous trees through most of the Qua- ternary. 0 1987 University of Washington. INTRODUCTION leoecological data were collected and most of the interpretations made. This paper is a In the late 1950s and early 1960s consid- critical reexamination of the chronology of erable research was conducted into the late the proposed pollen-analytical episodes Quaternary, principally late Pleistocene, and the interpretations of boreal forest for paleoecology of the Southern High Plains the region, made in light of recent advances of northwestern Texas and eastern New in palynology and radiocarbon dating and Mexico (Wendorf, 1961a; Wendorf and better understanding of the late Quaternary Hester, 1975a). One of the most significant geology, soils, and paleontology of the discoveries made, b,ased on considerable Southern High Plains and following on pollen data, was the high content of pine some points raised by Holliday er al.
    [Show full text]
  • Late Glacial to Early Holocene Climate Oscillations in the American Southwest Kenneth Cole, USGS Southwest Biological Science Center Flagstaff, AZ; Ken [email protected]
    Late Glacial to Early Holocene Climate Oscillations in the American Southwest Kenneth Cole, USGS Southwest Biological Science Center Flagstaff, AZ; [email protected] View of the Grand Canyon North Rim (2500 m) from a mid elevation (1500 m) on the South Rim. 1 Most of the earliest conceptions of the Pleistocene versus Holocene plant zonation consisted of lower Pleistocene zones and higher Holocene zones without much information on how they shifted from one to the other. 2 15,000 year-old packrat midden in a Grand Canyon cave. Steven’s Woodrat (Neotoma stevensii) poses with Kirsten Ironside. 3 Lower Colorado River Elevational Zonation Treeline Snowline 3000 Spruce Forest Treeline Modified From: Ponderosa Pine - Fir Forest Cole, K. L. 1990. Reconstruction Spruce Forest of past desert vegetation along the Colorado River using packrat 2000 middens. Palaeogeography, Palaeoclimatology, and Pinyon-Juniper Woodland Limber Pine, Fir Forest Palaeoecology 76: 349-366. Blackbrush - Sagebrush Juniper - Sagebrush Elevation (m) Desert Woodland 1000 Juniper - Ash Juniper - Blackbrush Brittle Bush - Woodland Woodland Creosote Bush Desert Joshua Tree - Brittle Bush - Creosote Bush Desert Sea Level Brittle Bush - Creosote Bush - Catclaw 0 5000 10000 15000 20000 Radiocarbon age (yr B.P.) K. Cole, 1995 This diagram shows a species individualistic approach made possible from plant macrofossils in packrat middens. There was still little information on the rapid Pleistocene to Holocene shift although intermediate plant assemblages were identified. 4 Carbon 13 values of packrat pellets from 92 fossil middens from the Grand Canyon, AZ Adapted From: Cole, K. L. and S. T. Arundel, 2005. Carbon 13 isotopes from fossil packrat pellets and elevational movements of Utah Agave reveal Younger Dryas cold period in Grand Canyon, Arizona.
    [Show full text]
  • 'Hyperdisease' Responsible for the Late Pleistocene Megafaunal Extinction?
    Ecology Letters, (2004) 7: 859–868 doi: 10.1111/j.1461-0248.2004.00643.x REPORT Was a ÔhyperdiseaseÕ responsible for the late Pleistocene megafaunal extinction? Abstract S. Kathleen Lyons,1* Felisa A. Numerous hypotheses have been proposed to explain the end Pleistocene extinction of Smith,1 Peter J. Wagner,2 Ethan large bodied mammals. The disease hypothesis attributes the extinction to the arrival of a P. White1 and James H. Brown1 novel ÔhyperdiseaseÕ brought by immigrating aboriginal humans. However, until West 1 Department of Biology, Nile virus (WNV) invaded the United States, no known disease met the criteria of a University of New Mexico, hyperdisease. We evaluate the disease hypothesis using WNV in the United States as a Albuquerque, NM 87131, USA model system. We show that WNV is size-biased in its infection of North America birds, 2Department of Geology, Field but is unlikely to result in an extinction similar to that of the end Pleistocene. WNV Museum of Natural History, infects birds more uniformly across the body size spectrum than extinctions did across Chicago, IL 60605, USA Present address: S. Kathleen mammals and is not size-biased within orders. Our study explores the potential impact Lyons, National Center for of WNV on bird populations and provides no support for disease as a causal mechanism Ecological Analysis and for the end Pleistocene megafaunal extinction. Synthesis, University of California – Santa Barbara, Keywords Santa Barbara, CA 93101, USA. Disease hypothesis, end-Pleistocene extinctions, mammals, megafauna, size-biased *Correspondence: E-mail: extinctions, West Nile virus. [email protected] Ecology Letters (2004) 7: 859–868 The disease hypothesis attributes the extinction of large INTRODUCTION mammals during the late Pleistocene to indirect effects of The mammalian faunas of Australia and the New World are the newly arrived aboriginal humans (MacPhee & Marx depauperate today.
    [Show full text]