The Quaternary of Virginia - a Symposium Volume

Total Page:16

File Type:pdf, Size:1020Kb

The Quaternary of Virginia - a Symposium Volume VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 75 THE QUATERNARY OF VIRGINIA - A SYMPOSIUM VOLUME Edited by J.N. McDonald and S.O. Bird COMMONWEALTH OF VIRGINIA DEPARTMENT OF MINES, MINERALS AND ENERGY DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVI LLE, VI RGIN IA 1 986 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 75 THE QUATERNARY OF VIRGINIA - A SYMPOSIUM VOLUME Edited by J.N. McDonald and S.O. Bird COMMONWEALTH OF VIRGINIA DEPARTMENT OF MINES, MINERALS AND ENERGY DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA 1 986 FRONT COVER: Quaternary travertine-marl deposits at Beaverdam Falls, Alleghany County. The falls are approximately 25 f.eet high (Photograph by David A. Hubbard, Jr.). VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 75 THE QUATERNARY OF VIRGINIA _ A SYMPOSIUM VOLUME Edited by J.N. McDonald and S.O. Bird COMMONWEALTH OF VIRGINIA DEPARTMENT OF MINES, MINERALS AND ENERGY DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVI LLE, VI RGINIA 1 986 DEPARTMENT OF MINES, MINERALS AND ENERGY RICHMOND. VIRGINIA O. GENE DISHNER. Director Commonwealth of Virginia, copyright 1986 FOREWARD River and some of its tributaries on selected headwater parts of the drainage basin by Kite, The Virginia Division of Mineral Resources Bell and Armstrong, and on travertine and marl celebrated the 150th anniversary of its founding deposits known from the state by Hubbard, Gi- in 1984 and 1985. One of several events sponsored annini and Lorah. Holman and Fay, in separate by the Division in commemoration of this anni- papers, present evidence that Pleistocene and versary was a Symposium on the Quaternary of modern assemblages of reptiles and amphibians Virginia, held in Charlottesville on September (herptiles) from middle Appalachian localities 26-28, 1984. This Symposium was designed to are harmonious, unlike those of mammals; herp- meet several important objeetives: to summarize tiles appear to have tolerated the extreme the state of knowledge on the Quaternary of ehanges in climate more easil5r than mammals. Virginia and its environs; to call attention to Changes in the composition of plant communities research underway on the Quaternary of Virginia in the Appalachians over the last 23,000 years and to identify problems, priorities, and direc- are described by Delcourt and Delcourt. Rem- tions for future work; to assemble scientists, nants of several Arctic and boreal plant species students and layman with interest and expertise which evidently became established in Virginia in the Quaternary of Virginia and its environs during glacial stages exist today in isolated areas in order to promote and facilitate the exchange near the summits of some of the State's higher of ideas and information on the subject; and to mountains as shown by Woodward and Ruska. promote new interest in the study of the Qua- Two recent studies of Pleistocene vertebrate fau- ternary of the region. The program provided a nas are included: one from a fissure-fill in Penn- comprehensive overview of the status of knowl- sylvania (Fonda and Czebieniak), the other from edge of the Quaternary of Virginia. Knowledge a fluvial (?) deposit in northern Virginia (Ott and about the megafauna of the region was empha- Weems). Eshelman and Grady give detailed des- sized in commemoration of Thomas Jefferson's criptions of Quaternary vertebrate localities in interest in this subject area. Virginia, ineluding lists of bird and mammal Eight of the thirteen invited papers and ten species found at these sites. McCary summarizes of the eleven poster papers presented at the some of his lifelong work on Paleo-Indians in Symposium are included in this volume. The Virginia by describing the distribution of Clovis keynote address presented by Silvio Bedini en- projectile points from around the State and notes titled "Thomas Jefferson and American Paleon- that nowhere in the State have ancient human tology" was published in 1985. The meeting closed activities been found in association with Pleis- with a field trip to Saltville led by Jerry McDo- tocene animal remains. Papers by White and nald (1984). Barfield summarize aspeets of recent archeolog- Contained in this volume are papers dealing ical investigations at one of the Saltville sites with many of the major topical areas of Quater- (aaSm5f). Rose uses archeologieal data and his- nary studies for Virginia and environs. A general torical accounts by early European observers to summary of geomorphic processes and an eval- document the occurrence and distribution of uation of evidence for Pleistocene overprints on large mammals in Virginia during the late pre- them are given by Conners, who finds a great historic and early historic period. McDonald need for detailed work on Pleistoeene geology in gives a historical sketeh of the development of Virginia. Three examples of geomorphic studies Quaternary vertebrate paleontology and zooar- ineluded in the present volume are those sum- cheology within Virginia, lists modern work un- marizing differences measured in fans on either derway on these topics, reviews some of the major side of the Blue Ridge by Kochel and Simmons features of ongoing field work at Saltville, and and on alluvial deposits lying above the Potomac recommends more emphasis on vertebrate pa- leontology and zooarcheology at Virginia univer- References sities and museums. A novel idea of Pleistocene extinctions, dwarfism, and deformity resulting Bedini, S., 1985, ThomasJefferson and American from inferred climate-induced decreases in blood paleontology: Virginia Division of Mineral supply to the mammalian uterus is presented by Resources Publieation 61,26 P. Mclean. Boaz recounts some of the early ideas Hoffer, F. B., 19??, Bibliography of Virginia on evolution of J. L. Cabell. geology and mineral resources-1960-1969: The editors here make readers aware of two Virginia Division of Mineral Resources Pub- important bibliographic works on the geology of lication 1, 68 p. Virginia, including those dealing with Quater- McDonald, J. N., 1984, The Saltville, Virginia nary geology, that mightotherwise be overlooked. locality: A summary of research and field trip One is the matchless product of a supreme effort guide: Charlottesville, Virginia Division of by J. K. Roberts (1942) and the other is a fine Mineral Resources 45 P. work eovering the decade from 1960 to 1969 by Roberts, J. K., 1942, Annotated geologieal bib- Boyd Hoffer (19??). We have compiled a new liographyof Virginia: Riehmond, Dietz Press, bibliography on the Quaternary of Virginia for 726p. those years to the present not included in the earlier cited works. This reference work was obtained from the GeoRef file of the Dialog Sys- tem in California. It is on open-file at the Virginia Division of Mineral Resourees and can be ob- tained by writing the Division Librarian. J. N. McDonald S. O. Bird, editors THE QUATERNARY OF VIRGINIA CONTENTS Invited Papers Page Quaternary geomorphic proeesses in Virginia, by John A. Conners 1 Late Quaternary vegetational change in the central Atlantie states, by Hazel R. Delcourt and Paul A. Delcourt Zg The known herpetofauna of the late Quanternary of Virginia poses Quaternary vertebrate localities of Virginia and their avian and mammalian fauna, by Ralph Eshelman and Frederick Grady 4g Early man in Virginia, by Ben C. McCary 7l Late prehistoric and protohistoric large mammal zoogeography of on the status of Quaternary vertebrate paleontologT and zooarcheology in Virginia, by Jerry N. McDonald ................. gg Embryogenesis dysfunction in the Pleistocene/Holoeene transition mammalian extinction, dwarfing, and skeletal abnormality, by Dewey M. Mclean .. .... rOb Abstracts of Poster Papers Preliminary observations on floodplain, terrace, and fan deposits in the upper Potomac River basin of virginia and west virginia, by J. steven Kite, Quaternary alluvial fans in central Virginia, by R. Craig Kochel and David W. Simmons ........................ 123 Quaternary travertine - marl deposits of virginia, by David A. Hubbard, Jr., William F. Giannini, and Michelle M. Lorah . .. ........ 126 wisconsinan herpetofaunas of the central Appalachians, by Leslie p. Fay ........... 126 Late Pleistocene fauna of the Hollidaysburg fissure, by shirley s. Fonda The Hot Run site: A new Pleistocene vertebrate locality in northern Virginia, by James R. Ott and Robert E. Weems .......l}g A Pleistocene legacy: Artic and boreal elements in the eontemporary biota of Virginia, by Susan L. Woodward and William F. Ruska, Jr. .............. ..:................... ........ 181 Projectile points from a multieomponent site (44Sm51) in the Saltville Valley, Tools anddebitage: Cultural debris from a multicomponent site (44Sm51) in the Saltville Valley, Virginia, by Eugene Barfield ..................... ........... 1BB Virginia's first evolutionist: James Lawrence Cabell, by N.T. Boaz .......... ... ....... l8b QUATERNARY GEOMORPHIC PROCESSES IN VIRGINIA John A. Connersr CONTENTS ?age Introduction ..............,.., Geomorphic processes and climatic change: problems and overview ................. 6 Processes of eavern and karst Suggestions for the Quaternary ILLUSTRATIONS Page Figure l: H"?;1,H1'#:"*;il'""1t#ffi'Hf,,;;;re;;, N",tn c"";ii;; : 3 3. view of northern slopes of Rich Mountain, showing foot-slope deposits g 4. Partof a seree slope near Sherando
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]
  • Mizzoualumnus1975novp16-19.Pdf (3.318Mb)
    THE GAUE THAT TRAPPED HISTORY Natural Trap Cave has been collecting bones of unwary animals for at least 13,000 years. Expeditions led by a Mizzou anthropologist are digging up those bones and clues about the cycles of climatic change. Text and Photos by Dave Holman IIi / m ISSOllRI ilLUrnrus The only entrenee to Natural Trap Ceve la the hole In the roof. Any enlmal that might have survived the fallatlll became a victim. Workera at theahe, below, ehherrappellnto theeave or descend theacafloldlng. A herd of small horses stampeded through the tall grass across a plateau near the edge of a canyon, pur­ sued by a large, long-legged cat. The cat closed on the slowest horse, forcing her along the canyon edge onto a peninsula of limestone. The cat sprang, fas­ tened its claws and teeth in the horse's neck, and suddenly, horse and cat disappeared from the face of the earth. Twelve thousand years later, a green panel truck and a dusty jeep bounced along a dirt road over the same plateau, now covered with sage and prickly pear. On the limestone peninsula where the horse and cat disappeared, the vehicles stopped by a 15- foot-wide hole in the rock. Eighty feet below is the floor of Natural Trap Cave. The cave floor is covered with the accumulated dust of centuries, clearly stratified and containing thou­ sands of bones of animals that failed to see the hole. This summer was the second consecutive year that Bob Gilbert, research associate in Mizzou's an­ thropology department had led an organized ex­ pedition to the trap.
    [Show full text]
  • Member Orientation Manual 2018
    Member Orientation Manual 2018 Fredericksburg Area Metropolitan Planning Organization 406 Princess Anne Street Fredericksburg, VA 22401 540.373.2890 www.fampo.gwregion.org 1 [THIS PAGE LEFT INTENTIONALLY BLANK] 2 TABLE OF CONTENTS GWRC/FAMPO Title VI Nondiscrimination Statement .................................................................................................. 5 FAMPO Mission Statement ............................................................................................................................................ 6 Chapter 1 introduction ............................................................................................................................................. 7 1.1 About the Fredericksburg Area Metroplitan Planning ORganization .................................................................. 7 PART I: OVERVIEW OF TRANSPORTATION PLANNING ................................................................................................... 8 What is the Transportation Planning Process? ......................................................................................................... 8 What is Performance-Based Planning? ..................................................................................................................... 9 What is a Metropolitan Planning Organization? ....................................................................................................... 9 What Other Responsibilities do Some MPOs Have? ..............................................................................................
    [Show full text]
  • Mammalia, Felidae, Canidae, and Mustelidae) from the Earliest Hemphillian Screw Bean Local Fauna, Big Bend National Park, Brewster County, Texas
    Chapter 9 Carnivora (Mammalia, Felidae, Canidae, and Mustelidae) From the Earliest Hemphillian Screw Bean Local Fauna, Big Bend National Park, Brewster County, Texas MARGARET SKEELS STEVENS1 AND JAMES BOWIE STEVENS2 ABSTRACT The Screw Bean Local Fauna is the earliest Hemphillian fauna of the southwestern United States. The fossil remains occur in all parts of the informal Banta Shut-in formation, nowhere very fossiliferous. The formation is informally subdivided on the basis of stepwise ®ning and slowing deposition into Lower (least fossiliferous), Middle, and Red clay members, succeeded by the valley-®lling, Bench member (most fossiliferous). Identi®ed Carnivora include: cf. Pseudaelurus sp. and cf. Nimravides catocopis, medium and large extinct cats; Epicyon haydeni, large borophagine dog; Vulpes sp., small fox; cf. Eucyon sp., extinct primitive canine; Buisnictis chisoensis, n. sp., extinct skunk; and Martes sp., marten. B. chisoensis may be allied with Spilogale on the basis of mastoid specialization. Some of the Screw Bean taxa are late survivors of the Clarendonian Chronofauna, which extended through most or all of the early Hemphillian. The early early Hemphillian, late Miocene age attributed to the fauna is based on the Screw Bean assemblage postdating or- eodont and predating North American edentate occurrences, on lack of de®ning Hemphillian taxa, and on stage of evolution. INTRODUCTION southwestern North America, and ®ll a pa- leobiogeographic gap. In Trans-Pecos Texas NAMING AND IMPORTANCE OF THE SCREW and adjacent Chihuahua and Coahuila, Mex- BEAN LOCAL FAUNA: The name ``Screw Bean ico, they provide an age determination for Local Fauna,'' Banta Shut-in formation, postvolcanic (,18±20 Ma; Henry et al., Trans-Pecos Texas (®g.
    [Show full text]
  • The Geologic Time Scale Is the Eon
    Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2.
    [Show full text]
  • Industrialism, Androids, and the Virtuoso Instrumentalist
    UNIVERSITY OF CALIFORNIA Los Angeles Performing the Mechanical: Industrialism, Androids, and the Virtuoso Instrumentalist A dissertation submitted in partial satisfaction of the requirements for the degree Doctor of Musical Arts by Leila Mintaha Nassar-Fredell 2013 © Copyright by Leila Mintaha Nassar-Fredell 2013 ABSTRACT OF THE DISSERTATION Performing the Mechanical: Industrialism, Androids, and the Virtuoso Instrumentalist by Leila Nassar-Fredell Doctor of Musical Arts University of California, Los Angeles, 2013 Professor Robert S. Winter, Chair Transactions between musical androids and actual virtuosos occupied a prominent place in the music of the eighteenth and nineteenth centuries. Instrumentalists and composers of instrumental music appropriated the craze for clockwork soloists, placing music in a position of increased social power in a society undergoing rapid technological transformation. The history of musical automata stretches back to antiquity. Androids and automata, vested by audiences with spiritual and magical qualities, populated the churches of the broader populations and the Renaissance grottos of the aristocracy. As ii the Industrial Revolution began, automata increasingly resembled the machines changing the structure of labor; consequently, androids lost their enchanted status. Contemporary writers problematized these humanoid machines while at the same time popularizing their role as representatives of the uncanny at the boundaries of human identity. Both instrumental performers and androids explored the liminal area between human and machine. As androids lost their magic, musical virtuosos assumed the qualities of spectacle and spirituality long embodied by their machine counterparts. In this process virtuosi explored the liminal space of human machines: a human playing a musical instrument (a machine) weds the body to a machine, creating a half-human, half-fabricated voice.
    [Show full text]
  • ABSTRACT JEWETT, AMANDA AVERELL. Aristocratic
    ABSTRACT JEWETT, AMANDA AVERELL. Aristocratic Gentlemanliness and Revolutionary Masculinities among Virginia’s Delegation to the Continental Congress, 1774-1776. (Under the direction of Dr. Craig Thompson Friend). There was never one type of manhood practiced in Virginia during from 1774 to 1776. Instead, different masculinities blended and overlapped to reflect changes in culture and society. While elements such as public validation and an honorable reputation persevered across gender constructions, they meant different things to different men in the early years of revolution. The American Revolution unleashed democratic, military, regional, and intellectual impulses that gave impetus to forms of manhood that helped to erode aristocratic gentlemanliness. Militant, intellectual, and southern men absorbed some ideals of aristocratic gentlemanliness like honor and public virtue, while abandoning others including submission and restraint. The Revolution and meetings with other men in the Continental Congress contributed to the dismissal of these principles as Virginians responded to changes in their political and social roles on a larger stage. Ultimately, the need for public approval ties all of these Virginians together. Validation of one’s gender and class from outside observers, be it fellow Virginian planters or delegates from other colonies, is the most permanent aspect of masculinity during these years. While other types of manhood—military, Enlightenment, and southern—broke from or changed several traits of aristocratic gentlemanliness,
    [Show full text]
  • Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia Emily Simpson East Tennessee State University
    East Tennessee State University Digital Commons @ East Tennessee State University Electronic Theses and Dissertations Student Works 5-2019 Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia Emily Simpson East Tennessee State University Follow this and additional works at: https://dc.etsu.edu/etd Part of the Paleontology Commons Recommended Citation Simpson, Emily, "Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia" (2019). Electronic Theses and Dissertations. Paper 3590. https://dc.etsu.edu/etd/3590 This Thesis - Open Access is brought to you for free and open access by the Student Works at Digital Commons @ East Tennessee State University. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of Digital Commons @ East Tennessee State University. For more information, please contact [email protected]. Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia ________________________________ A thesis presented to the faculty of the Department of Geosciences East Tennessee State University In partial fulfillment of the requirements for the degree Master of Science in Geosciences with a concentration in Paleontology _______________________________ by Emily Michelle Bruff Simpson May 2019 ________________________________ Dr. Chris Widga, Chair Dr. Blaine W. Schubert Dr. Andrew Joyner Key Words: Paleoecology, land-use, grassy balds, stable isotope ecology, Whitetop Mountain ABSTRACT Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia by Emily Michelle Bruff Simpson Land-use, feeding habits, and response to seasonality by Quaternary megaherbivores in Saltville, Virginia, is poorly understood. Stable isotope analyses of serially sampled Bootherium and Equus enamel from Saltville were used to explore seasonally calibrated (δ18O) patterns in megaherbivore diet (δ13C) and land-use (87Sr/86Sr).
    [Show full text]
  • Occurrence of the Musk Ox, Symbos Cavifrons, from Southeastern Idaho and Comments on the Genus Bootherium
    Great Basin Naturalist Volume 47 Number 2 Article 9 4-30-1987 Occurrence of the musk ox, Symbos cavifrons, from southeastern Idaho and comments on the genus Bootherium Michael E. Nelson Fort Hays State University, Hays, Kansas James H. Madsen Jr. Antiquities Section, Utah Division of State History, Salt Lake City Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Nelson, Michael E. and Madsen, James H. Jr. (1987) "Occurrence of the musk ox, Symbos cavifrons, from southeastern Idaho and comments on the genus Bootherium," Great Basin Naturalist: Vol. 47 : No. 2 , Article 9. Available at: https://scholarsarchive.byu.edu/gbn/vol47/iss2/9 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. OCCURRENCE OF THE MUSK OX, SYMBOS CAVIFRONS, FROM SOUTHEASTERN IDAHO AND COMMENTS ON THE GENUS BOOTHERIUM Michael E. Nelson' and James H. Madsen, Jr." Abstract.—A set of ovibovine horn cores collected from Pleistocene sediments in southeastern Idaho provides additional evidence for sexual dimorphism in the helmeted musk ox, Symhos cavifrons. Specimens previously assigned to Boothchum sargenti are placed in synonomy with Symbos cavifrons as sexual dimorphs (females). Bootherium bomhifrons is a \alid taxon and is probably not closely related to Symbos. The taxonomic status of the e.xtinct musk figures and descriptions, pronounced that ox, Bootherium, has been questioned since Bootherium cavifrons (= Symbos cavifrons) Leidy (1852a, 1852b) proposed the name for was a male and B.
    [Show full text]
  • Mesofauna at the Soil-Scree Interface in a Deep Karst Environment
    diversity Article Mesofauna at the Soil-Scree Interface in a Deep Karst Environment Nikola Jureková 1,* , Natália Raschmanová 1 , Dana Miklisová 2 and L’ubomír Kováˇc 1 1 Department of Zoology, Institute of Biology and Ecology, Faculty of Science, Pavol Jozef Šafárik University in Košice, Šrobárova 2, SK-04180 Košice, Slovakia; [email protected] (N.R.); [email protected] (L’.K.) 2 Institute of Parasitology, Slovak Academy of Sciences, Hlinkova 3, SK-04001 Košice, Slovakia; [email protected] * Correspondence: [email protected] Abstract: The community patterns of Collembola (Hexapoda) were studied at two sites along a microclimatically inversed scree slope in a deep karst valley in the Western Carpathians, Slovakia, in warm and cold periods of the year, respectively. Significantly lower average temperatures in the scree profile were noted at the gorge bottom in both periods, meaning that the site in the lower part of the scree, near the bank of creek, was considerably colder and wetter compared to the warmer and drier site at upper part of the scree slope. Relatively high diversity of Collembola was observed at two fieldwork scree sites, where cold-adapted species, considered climatic relicts, showed considerable abundance. The gorge bottom, with a cold and wet microclimate and high carbon content even in the deeper MSS horizons, provided suitable environmental conditions for numerous psychrophilic and subterranean species. Ecological groups such as trogloxenes and subtroglophiles showed decreasing trends of abundance with depth, in contrast to eutroglophiles and a troglobiont showing an opposite distributional pattern at scree sites in both periods. Our study documented that in terms of soil and Citation: Jureková, N.; subterranean mesofauna, colluvial screes of deep karst gorges represent (1) a transition zone between Raschmanová, N.; Miklisová, D.; the surface and the deep subterranean environment, and (2) important climate change refugia.
    [Show full text]
  • Quaternary Records of the Dire Wolf, Canis Dirus, in North and South America
    Quaternary records of the dire wolf, Canis dirus, in North and South America ROBERT G. DUNDAS Dundas, R. G. 1999 (September): Quaternary records of the dire wolf, Canis dirus, in North and South Ameri- ca. Boreas, Vol. 28, pp. 375–385. Oslo. ISSN 0300-9483. The dire wolf was an important large, late Pleistocene predator in North and South America, well adapted to preying on megaherbivores. Geographically widespread, Canis dirus is reported from 136 localities in North America from Alberta, Canada, southward and from three localities in South America (Muaco, Venezuela; Ta- lara, Peru; and Tarija, Bolivia). The species lived in a variety of environments, from forested mountains to open grasslands and plains ranging in elevation from sea level to 2255 m (7400 feet). Canis dirus is assigned to the Rancholabrean land mammal age of North America and the Lujanian land mammal age of South Amer- ica and was among the many large carnivores and megaherbivores that became extinct in North and South America near the end of the Pleistocene Epoch. Robert G. Dundas, Department of Geology, California State University, Fresno, California 93740-8031, USA. E-mail: [email protected]; received 20th May 1998, accepted 23rd March 1999 Because of the large number of Canis dirus localities Rancho La Brea, comparing them with Canis lupus and and individuals recovered from the fossil record, the dire wolf specimens from other localities. Although dire wolf is the most commonly occurring large knowledge of the animal’s biology had greatly predator in the Pleistocene of North America. By increased by 1912, little was known about its strati- contrast, the species is rare in South America.
    [Show full text]
  • Guidebook Contains Preliminary Findings of a Number of Concurrent Projects Being Worked on by the Trip Leaders
    TH FRIENDS OF THE PLEISTOCENE, ROCKY MOUNTAIN-CELL, 45 FIELD CONFERENCE PLIO-PLEISTOCENE STRATIGRAPHY AND GEOMORPHOLOGY OF THE CENTRAL PART OF THE ALBUQUERQUE BASIN OCTOBER 12-14, 2001 SEAN D. CONNELL New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave. SE, Albuquerque, New Mexico 87106 DAVID W. LOVE New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 JOHN D. SORRELL Tribal Hydrologist, Pueblo of Isleta, P.O. Box 1270, Isleta, NM 87022 J. BRUCE J. HARRISON Dept. of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 Open-File Report 454C and D Initial Release: October 11, 2001 New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 NMBGMR OFR454 C & D INTRODUCTION This field-guide accompanies the 45th annual Rocky Mountain Cell of the Friends of the Pleistocene (FOP), held at Isleta Lakes, New Mexico. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually in the field. The field guide has been separated into two parts. Part C (open-file report 454C) contains the three-days of road logs and stop descriptions. Part D (open-file report 454D) contains a collection of mini-papers relevant to field-trip stops. This field guide is a companion to open-file report 454A and 454B, which accompanied a field trip for the annual meeting of the Rocky Mountain/South Central Section of the Geological Society of America, held in Albuquerque in late April.
    [Show full text]