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Late Pliocene-Early Pleistocene Ecologic Changes in the Arctic Ocean Borderland

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Late Pliocene-Early Pleistocene Ecologic Changes in the Arctic Ocean Borderland Late Pliocene-Early Pleistocene Ecologic Changes in the Arctic Ocean Borderland I U.S. GEOLOGICAL SURVEY BULLETIN 2036 AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated monthly, which is for sale in microfiche from the USGS ESIC-Open-File Report Sales, Box 25286, Building 810, Denver Federal Center, Denver, CO 80225 Order U.S. Geological Survey publications by mail or over the counter from the offices given below. 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Subscriptions to periodicals (Earthquakes & Volcanoes and • RESTON, Virginia-National Center, Rm. 1C402, 12201 Preliminary Determination of Epicenters) can be obtained ONLY Sunrise Valley Dr. from • SALT LAKE CITY, Utah-Federal Bldg., Rm. 8105, 125 South State St. Superintendent of Documents U.S. Government Printing Office • SPOKANE, Washington-U.S. Courthouse, Rm. 678, West Washington, DC 20402 920 Riverside Ave. • WASHINGTON, D.C.-U.S. Department of the Interior Bldg., (Check or money order must be payable to Superintendent of Rm. 2650, 1849 C St., NW. Documents.) Maps Maps Maps may be purchased over the counter at the U.S. Geolog­ For maps, address mail order to ical Survey offices where books are sold (all addresses in above list) and at the following Geological Survey offices: USGS Map Distribution Box 25286, Building 810 Denver Federal Center • ROLLA, Missouri-1400 Independence Rd. Denver, CO 80225 • FAIRBANKS, Alaska-New Federal Building, 101 Twelfth Ave. Residents of Alaska may order maps from U.S. Geological Survey, Map Sales 101 Twelfth Ave., Box 12 Fairbanks, AK 99701 Late Pliocene-Early Pleistocene Ecologic Changes in the Arctic Ocean Borderland By CHARLES A. REPENNING and ELISABETH M. BROUWERS U.S. GEOLOGICAL SURVEY BULLETIN 2036 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Any use of trade, product, or finn names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Repenning, Charles Albert, 1922- Late Pliocene-Early Pleistocene ecologic changes in the Arctic Ocean Borderland I by Charles A. Repenning and Elisabeth M. Brouwers. p. cm.-(U.S. Geological Survey bulletin ; 2036) Includes bibliographical references. Supt. of Docs. no.: I 19.3:2036 1. Paleoecology-Arctic regions. I. Brouwers, Elisabeth M. II. Title. III. Series. QE75.B9 no. 2036 [QE720] 557.3 s-dc20 92-23139 [560'.45] CIP CONTENTS Abstract................................................................................................................................. 1 Introduction........................................................................................................................... 2 Age Assignments........................................................................................................ 5 Isotope and Polarity Records...................................................................................... 6 Aoral Terms................................................................................................................ 6 3.0--2.0 Million Years Ago: The First Cooling Cycle.......................................................... 8 Canada, Meighen Island: Beaufort Formation............................................................ 8 Alaskan North Slope: Gubik Formation..................................................................... 9 Colvillian and Bigbendian Transgressions ........................................................... 9 Fishcreekian "Transgression"............................................................................... 10 Yakutia: Begunov Suite and Kutuyakh Beds....................................................... 13 Marine and Proxy Records of the First Cooling Cycle......................................................... 15 Norwegian Sea: Scandinavian Ice Sheet.................................................................... 15 Central Arctic Ocean: Eastern Alpha Ridge............................................................... 17 Western Arctic Ocean: Mendeleyev Ridge ............... .. ... .......... ..... ....... .. .... .. ............ .. 18 Summary of the First Cooling Cycle.................................................................................... 18 2.0--0.85 Million Years Ago: The Second Cooling Cycle.................................................... 20 Greenland: Kap KS?Sbenhavn Formation................................................................................ 20 Y akutia: Krestovka Olyor Suite.................................................................................. 22 Yakutia: Type Olyor Suite.......................................................................................... 24 Alaska: Cape Deceit Section ........ .. ......... .. .. .. ..... ....... ...... ............ ...... ....... .. ........... 25 Canada: Yukon Territory-Locality CRH-47 ........................................................... 27 Marine and Proxy Records of the Second Cooling Cycle ........ ... .. .. ...... ... .. ..... ..... ........ 27 Norwegian Sea: Scandinavian Ice Sheet.................................................................... 28 Microtine Immigrants: Western United States..................................................................... 28 First Cooling Cycle..................................................................................................... 29 Beginning of the Second Cooling Cycle . .. ..... .. ....... ........... ................ ............ .......... .. 29 Eburonian Cold........................................................................................................... 30 Beginning of the Ice Ages .. ..... ............. .. ........ .. ..... ...... ...... ....... ... .. ............ ......... .. .. 31 Summary: Late Pliocene-Early Pleistocene Ecologic Change............................................ 32 References Cited................................................................................................................... 34 FIGURES 1. Map showing localities discussed in text........................................................................................................................ 3 2. Diagram showing correlation of localities and events discussed in text ............. .............. ... .. .... ...... ...... .... .................. 7 TABLE 1. Pollen from the Bigbendian deposits, Alaskan North Slope, compared with pollen from the Begunov Suite, Yakutia 13 III LATE PLIOCENE-EARLY PLEISTOCENE ECOLOGIC CHANGES IN THE ARCTIC OCEAN BORDERLAND By CHARLES A. REPENNING1 and ELISABETH M. BROUWERS1 ABSTRACT Between 3.0 and 0.85 million years ago the Arctic and depositional records from the central part of the Arctic Ocean Borderland experienced two cycles of climatic dete­ Ocean indicate that this lack of ice cover may not have rioration, both of which ended in major Northern Hemi­ extended to the pole; from about 2.48 until about 2.1 mil­ sphere continental glaciation. The first cooling cycle ended lion years ago perennial ice cover is thought to have 2.1 million years ago; continental ice extended down the formed intermittently in the central Arctic Ocean. There Mississippi River Valley as far south as Iowa. The cooling are no known terrestrial records in the Arctic Ocean Bor­ cycle was followed by a collapse of glaciation and an derland for much of the time of this first intermittent peren­ extremely warm climate that extended to the northernmost nial sea ice; however, both sediments and fauna from the land, almost to the North Pole. This warmth at the begin­ beginning and from the end of this period indicate that ice ning of the second cooling cycle was
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