Last edited by Samulabar
Tuesday, August 18, 2020 | History

2 edition of Quaternary stratotypes of North America found in the catalog.

Quaternary stratotypes of North America

Quaternary stratotypes of North America

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Published by Quaternary Sciences Institute, University of Waterloo in Waterloo, Ont .
Written in English

    Subjects:
  • Geology, Stratigraphic -- Quaternary.,
  • Geology -- Canada.,
  • Geology -- United States.

  • Edition Notes

    StatementThe Subcommission on North American Quaternary Stratigraphy, International Union for Quaternary Research (INQUA) ; [P.F. Karrow, editor].
    SeriesQ.S.I. publication -- no. 8
    ContributionsKarrow, P. F., 1930-, International Union for Quaternary Research. Subcommission on North American Quaternary Stratigraphy., University of Waterloo. Quaternary Sciences Institute.
    The Physical Object
    Paginationv.
    ID Numbers
    Open LibraryOL16052809M
    ISBN 100969563310
    OCLC/WorldCa28669397

      1. Introduction. During the Late Pleistocene and early Holocene, regions around the world suffered losses of megafauna species of a magnitude unprecedented for many millions of years [1–3].Although extinctions are common in the Quaternary fossil record, such rapid and large global species losses without functional replacements are unusual.   This book is the first annotated bibliography of Quatenary vertebrates of Canada, Alaska, and Greenland. It focuses on highlights (species mentioned, locality, geological age, stratigraphic positions, etc.) of nearly items published between and , dealing with the remains of fishes, amphibians, reptiles and, mainly, mammals that lived from about 2 million to five thousand .

    Although Bonnicksen's enthusiasm for forestry and Native American history shines through, his tendency to overstate the influence of the latter on the former keeps the book from being a definitive history of late-Quaternary ecology in North America. Such a book does not yet exist, although Pielou () provides a good general introduction. This book is the second of three volumes in which the recent knowledge of the extent and chronology of Quaternary glaciations has been compiled on a global scale. This information is seen as a fundamental requirement, not only for the glacial community, but for the wider user-community of general Quaternary .

    Quaternary - Quaternary - Quaternary life: The length of the Quaternary is short relative to geologic and evolutionary time scales, but the rate of evolutionary change during this period is high. It is a basic tenet of ecology that disturbance increases diversity and ultimately leads to evolutionary pressures. The Quaternary is replete with forces of disturbance and evidence for evolution in. Quaternary (/ k w ə ˈ t ɜːr n ə r i, ˈ k w ɒ t. ər ˌ n ɛr. i / kwə-TUR-nə-ree, KWOT-ər-nerr-ee) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from ± million years ago to the present. The Quaternary Period is divided into.


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Quaternary stratotypes of North America Download PDF EPUB FB2

General Information. Title: Quaternary stratotypes of North America; Volume 1 Author(s): Karrow, P.F. (editor) Publishing Organization: University of Waterloo, Quaternary Sciences Institute Series and Number: Publication no.

8 [p. ] Publication Date: Cross Section: None North Latitude: 49° 0' 5" N () South Latitude: 31° 19' 57" N (). Indeed, for many I am sure that it will form the catalyst for further research endeavours on Quaternary glaciation in North America.

Each chapter provides me with an updated compilation of the state of the art for specific areas of North America, written by researchers who are actively involved in reconstructing Quaternary glaciations.

COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has pulled together information and resources to assist library staff as they consider how to handle coronavirus.

In North America, the fundamental units of geological-climate classification have been defined as follows (American Commission on Stratigraphic Nomenclature ): ‘A glaciation is a climatic episode during which extensive glaciers developed, attained a maximum extent, and receded.

A stadial is a climatic episode, representing a subdivision. A. DreimanisMiddle Wisconsin substage in its type region, the eastern Great Lakes, Ohio River basin, North America Quaternary Studies in Poland, 3 (), pp. Google ScholarCited by: This book reviews advances in understanding Quaternary stratotypes of North America book the past ca.

two million years of Earth history - the Quaternary Period - in the United States. It begins with sections on ice and water - as glaciers, permafrost, oceans, rivers, lakes, and aquifers. Six chapters are devoted to the high-latitude Pleistocene ice sheets, to mountain glaciations of the western United States, and to permafrost studies.3/5(1).

Quaternary stratotypes of North America by Paul Frederick Karrow Published by Published For The Submission By The Quaternary Sciences Institute ISBNISBN: Geologia aplicada a la ingenieria civil by Robert F. Tertiary Period - Tertiary Period - Tertiary rocks: Classically, the Cenozoic Era was divided into the Tertiary and Quaternary periods, separated at the boundary between the Pliocene and Pleistocene epochs (formerly set at million years ago); however, by the late 20th century many authorities considered the terms Tertiary and Quaternary to be obsolete.

The Quaternary period (from ± million years ago to the present) saw the extinctions of numerous predominantly megafaunal species, which resulted in a collapse in faunal density and diversity and the extinction of key ecological strata across the globe.

The most prominent event in the Late Pleistocene is differentiated from previous Quaternary pulse extinctions by the widespread. Neogene molluscan stages of the West Coast of North America.

Palaeogeogr., Palaeoclimatol., Palaeoecol., Neogene marine sediments of the West Coast of North America were deposited in a series of widely spaced basins that extended geographically from the western and northern Gulf of Alaska (60) to southern California (33).

Wikimedia Commons. Modern horses have come a long way since their prehistoric ancestors roamed the grasslands and prairies of Cenozoic North America. On the following slides, you'll find pictures and detailed profiles of over a dozen prehistoric horses, ranging from the American Zebra to.

Contents was published in Annotated Bibliography of Quaternary Vertebrates of Northern North America on page vii. In North America, mainly in the USA, the term interglaciation is occasionally used for interglacial (cf. American Code ). Likewise, the terms stade and interstade may be used instead of stadial and interstadial, respectively (cf.

American Code ). Speleothem oxygen isotope records from the Caribbean, Central, and North America reveal climatic controls that include orbital variation, deglacial forcing related to ocean circulation and ice sheet retreat, and the influence of local and remote sea surface temperature variations.

Here, we review these records and the global climate teleconnections they suggest following the recent publication. The American Quaternary Association: The American Quaternary Association (AMQUA) is a professional organization of North American scientists devoted to studying all aspects of the Quaternary Period, about the last 2 million years of Earth history.

Top of List. Colleges and Universities (showing 1 of 1 listings). Karrow, P.F. (editor),Quaternary stratotypes of North America; Volume 1: University of Waterloo, Quaternary Sciences Institute Publication, no. 8, p.Prepared for the Subcommission on North American Stratigraphy, International Union for Quaternary Research (INQUA).

Summaries of the major features of the geology of North America and the adjacent oceanic regions are presented. Twenty chapters include concise reviews of current thinking about Precambrian basement, Phanerozoic orogens, cratonic basins, passive-margin geology of the Atlantic and Gulf Coast regions, marine and terrestrial geology of the Caribbean region, marine geology of the North Atlantic.

Submerged paleoshorelines, ubiquitous across humid regions, reveal that North America's ecosystems and critical zone existed in a drier‐than‐modern state for much of the Quaternary and that continental moisture gradients often differed from today.

The hydrologic changes underscore the climatic risk to many societally critical water supplies. This book examines case studies of North American Quaternary mammalian evolution within the larger domain of modern evolutionary theory.

The book presents previously unpublished studies of a variety of taxa (xenarthrans, rodents, carnivores, ungulates) examined over several temporal scales, from a few thousand years during the Holocene to.

This book is the second of three volumes in which the recent knowledge of the extent and chronology of Quaternary glaciations has been compiled on a global scale. This information is seen as a fundamental requirement, not only for the glacial community, but for the wider user-community of general Quaternary workers.

In particular the need for accurate ice-front positions is a basic requirement. In North America only a few Pleistocene insect fossils have been studied so that it is impossible to bring together syntheses comparable to those made for parts of Europe (Coopeet al., ; Pearson, ).

Because of this sparse fossil information, present contributions, to a knowledge of the Pleistocene through the study of North American.The Pliocene: time of change: including papers from the symposium entitled "The palynology, climate and sequence stratigraphy of the Pliocene" (held during the 26th annual meeting of the American Association of Stratigraphic Palynologists, Inc., Baton Rouge, Louisiana, ) (Book).Five auxiliary stratotypes for the Pleistocene-Holocene boundary have also been recognised.

(c) Walker et al.Journal of Quaternary Science, 24, p.John Wiley & Sons, Ltd. Digital Object Identifier (DOI) /jqs