Skip to main content

Advertisement

Log in

Tundra and boreal forest of interior Alaska during terminal MIS 6 and MIS 5e

  • Original Article
  • Published:
Vegetation History and Archaeobotany Aims and scope Submit manuscript

Abstract

Two sites within the boreal forest of interior Alaska shed light on the climate and vegetation of terminal marine isotope stage (MIS) 6 (ca. 140–130 kyr ago) and MIS 5e (125–116 kyr ago). The Birch Creek and Koyukuk localities are river-cut exposures with sediments dating from the penultimate glaciation (at least) to the present. Plant macrofossils, pollen, and beetles were analyzed at these sites. Terminal MIS 6-aged samples indicate a cooler than modern climate and the presence of shrub tundra. During MIS 5e, boreal forest grew at the sites and temperatures were similar to modern times. However, the forest may also have been more mesic than today, as indicated by relatively abundant ferns. Winters may have been warmer than today, as suggested by beetle-based climatic reconstructions as well as the presence of two extralimital taxa that today live in regions where winter temperatures are up to 15 °C warmer than at the site localities.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Anderberg A-L (1994) Atlas of seeds and small fruits of Northwest European plant species part 4: resedaceae-umbelliferae. Swedish Museum of Natural History, Stockholm

    Google Scholar 

  • Anderson PM, Edwards ME, Brubaker LB (2004) Results and paleoclimate implications of 35 years of paleoecological research in Alaska. In: Gillespie AR, Porter SC (eds) The quaternary period in the United States. Elsevier, Amsterdam, pp 427–440

    Google Scholar 

  • Andreev AA, Grosse G, Schirrmeister L, Kuzmina SA, Novenko EY, Bobrov AA, Tarasov PE, Ilyashuk BP, Kuznetsova TV, Krbetschek M, Meyer H, Kunitsky VV (2004) Late saalian and eemian palaeoenvironmental history of the Bol’shoy Lyakhovsky Island (Laptev Sea region, Arctic Siberia). Boreas 33:319–348. doi:10.1111/j.1502-3885.2004.tb01244.x

    Article  Google Scholar 

  • Atkinson TC, Briffa KR, Coope GR, Joachim M, Perry D (1986) Climatic calibration of coleopteran data. In: Berglund BE (ed) Handbook of holocene palaeoecology and palaeohydrology. Wiley, London, pp 851–858

    Google Scholar 

  • Axford Y, Briner JP, Francis, Miller GH, Walker IR, Wolfe AP (2011) Chironomids record terrestrial temperature changes throughout arctic interglacials of the past 200,000 yr. Geol Soc Am Bull 123:1,275–1,287. doi:10.1130/b30329.1

    Article  Google Scholar 

  • Bartlein PJ, Lipsitz B, Thompson RS (1994) Modern climate data for paleoenvironmental interpretations. American quaternary association thirteenth biennial meeting, p 197

  • Begét J, Edwards ME, Hopkins D, Keskinen M, Kukla G (1991) Old Crow tephra at the palisades of the Yukon, Alaska. Quat Res 35:291–297

    Article  Google Scholar 

  • Bennike O, Böcher J (1994) Land biotas of the last interglacial/glacial cycle on Jameson Land, East Greenland. Boreas 23:479–487

    Article  Google Scholar 

  • Berger GW, Anderson PM, Anderson PM (2000) Extending the geochronometry of arctic lake cores beyond the radiocarbon limit by using thermoluminescence. J Geophys Res 105:15,439–15,455

    Article  Google Scholar 

  • Berggren G (1969) Atlas of seeds and small fruits of Northwest European plant species part 2: cyperaceae. Swedish Natural Science Research Council, Stockholm

    Google Scholar 

  • Berggren G (1981) Atlas of seeds and small fruits of Northwest European plant species part 3: salicaceae-cruciferae. Swedish Museum of Natural History, Stockholm

    Google Scholar 

  • Birks HH (2007) Plant macrofossil introduction. In: Elias SA (ed) Encyclopedia of Quaternary science. Elsevier, Amsterdam, pp 2,266–2,288

    Chapter  Google Scholar 

  • Birks HH, Birks HJB (2000) Future uses of pollen analysis must include plant macrofossils. J Biogeogr 27:31–35

    Article  Google Scholar 

  • Bray PJ, Blockley SPE, Coope GR, Dadswell LF, Elias SA, Lowe JJ, Pollard AM (2006) Refining mutual climatic range (MCR) quantitative estimates of palaeotemperature using ubiquity analysis. Quat Sci Rev 25:1,865–1,876. doi:10.1016/j.quascirev.2006.01.023

    Article  Google Scholar 

  • Brayshaw TC (2000) Pondweeds, bur-reeds and their relatives of British Columbia. Royal British Columbia Museum, Victoria

    Google Scholar 

  • Bright DE (1976) Bark beetles of Canada and Alaska (coleoptera: scolytidae). The insects and arachnids of Canada, part 2. Department Of Agriculture publication 1576. Canada Department of Agriculture, Ottawa

    Google Scholar 

  • Campbell JM (1983) A revision of the North American omaliinae (coleoptera: staphylinidae): the genus olophrum Erichson. Can Entomol 115:577–622

    Article  Google Scholar 

  • Campbell JM (1984) A revision of the North American omaliinae (coleoptera: staphylinidae): the genera Arpedium Erichson and Eucnecosum Reitter. Can Entomol 116:487–527

    Article  Google Scholar 

  • CAPE Last Interglacial Project Members (2006) Last interglacial arctic warmth confirms polar amplification of climate change. Quat Sci Rev 25:1,383–1,400

    Article  Google Scholar 

  • Douglas GW, Meidinger D, Pojar J (2001) Illustrated flora of British Columbia: volume 6 monocotyledons (acoraceae through Najadaceae). British Columbia ministry of environment, lands, and parks and British Columbia ministry of forests, Victoria

  • Edwards ME, McDowell PF (1989) Quaternary deposits at Birch Creek, northeastern interior Alaska: the possibility of climatic reconstruction. In: Carter LD, Hamilton TD, Galloway JP (eds) Late cenozoic history of the interior basins of Alaska and the Yukon. U.S. geological survey circular 1026. US Geological Survey, Washington

    Google Scholar 

  • Edwards ME, McDowell PF (1991) Interglacial deposits at Birch Creek, northeast interior Alaska. Quat Res 35:41–52

    Article  Google Scholar 

  • Edwards ME, Bigelow NH, Finney BP, Eisner WR (2000) Records of aquatic pollen and sediment properties as indicators of late-Quaternary Alaskan lake levels. J Paleolimnol 24:55–68

    Article  Google Scholar 

  • Edwards ME, Hamilton TD, Elias SA, Bigelow NH, Krumhardt AP (2003) Interglacial extension of the boreal forest limit in the Noatak valley, northwest Alaska: evidence from an exhumed river-cut bluff and debris apron. Arct Antarct Alp Res 35:460–468

    Article  Google Scholar 

  • Ehlers J, Gibbard P (2008) Extent and chronology of Quaternary glaciation. Episodes 31:211–218

    Google Scholar 

  • Elias SA (1994) Quaternary insects and their environments. Smithsonian Institution Press, Washington

    Google Scholar 

  • Elias SA (2001) Mutual climatic range reconstructions of seasonal temperatures based on late Pleistocene fossil beetle assemblages in Eastern Beringia. Quat Sci Rev 20:77–91

    Article  Google Scholar 

  • Elias SA (2007) Beetle records overview. In: Elias SA (ed) Encyclopedia of Quaternary science. Elsevier, Oxford, pp 153–163. doi:10.1016/B0-44-452747-8/00270-2

    Chapter  Google Scholar 

  • Esat TM, McCulloch MT, Chappell J, Pillans B, Omura A (1999) Rapid fluctuations in sea level recorded at Huon Peninsula during the penultimate deglaciation. Science 283:197–201

    Article  Google Scholar 

  • Fægri K, Iversen J (1989) Textbook of pollen analysis, 4th edn. Wiley, Chichester

    Google Scholar 

  • Finnamore A (2000) Alberta forest biodiversity monitoring program, arthropod pilot study. http://abmi.biology.ualberta.ca/18_Chapter_Compendium/Arthropod%20Pilot%20Study_15.pdf. Accessed 11 Oct 2006

  • Flora of North America Editorial Committee (2000) Flora of North America North of Mexico. Magnoliophyta: Alismatidae, Arecidae, Commelinidae (in part), and Zingiberidae, vol 22. Oxford University Press, Oxford

    Google Scholar 

  • Francis DL, Wolfe AP, Walker IR, Miller GH (2006) Interglacial and Holocene temperature reconstructions based on midge remains in sediments of two lakes from Baffin Island, Nunavut, Arctic Canada. Palaeogeogr Palaeoclim Palaeoecol 236:107–125

    Article  Google Scholar 

  • Frechette B, Wolfe AP, Miller GH, Richard PJH, De Vernal A (2006) Vegetation and climate of the last interglacial on Baffin Island, Arctic Canada. Palaeogeogr Palaeoclim Palaeoecol 236:91–106. doi:10.1016/j.palaeo.2005.11.034

    Article  Google Scholar 

  • Gallup CD, Cheng H, Taylor FW, Edwards RL (2002) Direct determination of the timing of sea level change during termination II. Science 295:310–313. doi:10.1126/science.1065494

    Article  Google Scholar 

  • Hamilton TD, Brigham-Grette J (1991) The last interglaciation in Alaska: stratigraphy and paleoecology of potential sites. Quat Int 10–12:49–71

    Article  Google Scholar 

  • Harrison SP, Digerfeldt G (1993) European lakes as palaeohydrological and palaeoclimatic indicators. Quat Sci Rev 12:233–248

    Article  Google Scholar 

  • Hultén E (1968) Flora of Alaska and neighboring territories. Stanford University Press, Stanford

    Google Scholar 

  • Imbrie J, Berger A, Boyle EA, Clemens SC, Duffy A, Howard WR, Kukla G, Kutzbach J, Martinson DG, McIntyre A, Mix AC, Molfino B, Morley JJ, Peterson LC, Pisias NG, Prell WL, Raymo ME, Shackelton NJ, Toggweiler JR (1993) On the structure and origin of major glaciation cycles 2. The 100,000-year cycle. Paleoceanography 8:699–735

    Article  Google Scholar 

  • Johnstone JF, Chapin FS, Hollingsworth TN, Mack MC, Romanovsky V, Turetsky M (2010) Fire, climate change, and forest resilience in interior Alaska. Can J Forest Res 40:1,302–1,312. doi:10.1139/X10-061

    Article  Google Scholar 

  • Katz NJ, Katz SV, Kipiani MG (1965) Atlas and keys of fruits and seeds occurring in the Quaternary deposits of the USSR (in Russian). Nauka, Moscow

    Google Scholar 

  • Kaufman DS, Ager TA, Anderson NJ, Anderson PM, Andrews JT, Bartlein PJ, Brubaker LB, Coats LL, Cwynar LC, Duvall ML, Dyke AS, Edwards ME, Eisner WR, Gajewski K, Geirsdóttir A, Hu FS, Jennings AE, Kaplan MR, Kerwin MW, Lozhkin AV, MacDonald GM, Miller GH, Mock CJ, Oswald WW, Otto-Bleisner BL, Porinchu DF, Rühland K, Smol JP, Steig EJ, Wolfe BB (2004) Holocene thermal maximum in the western Arctic (0–180°W). Quat Sci Rev 23:529–560

    Article  Google Scholar 

  • Kelly R, Chipman ML, Higuera PE, Stefanova I, Brubaker LB, Hu FS (2013) Recent burning of boreal forests exceeds fire regime limits of the past 10,000 years. Proc Nat Acad Sci. doi:10.1073/pnas.1305069110

    Google Scholar 

  • Kienast F, Tarasov P, Schirrmeister L, Grosse G, Andreev AA (2008) Continental climate in the east Siberian Arctic during the last interglacial; implications from palaeobotanical records. Glob Planet Change 60:535–562. doi:10.1016/j.gloplacha.2007.07.004

    Article  Google Scholar 

  • Kienast F, Wetterich S, Kuzmina S, Schirrmeister L, Schirrmeister L, Andreev AA, Tarasov P, Nazarova L, Kossler A, Frolova L, Kunitsky VV (2011) Paleontological records indicate the occurrence of open woodlands in a dry inland climate at the present-day Arctic coast in western Beringia during the last interglacial. Quat Sci Rev 30:2,134–2,159. doi:10.1016/j.quascirev.2010.11.024

    Article  Google Scholar 

  • Kuzmina S, Elias S, Matheus P, Storer JE, Sher A (2008) Paleoenvironmental reconstruction of the last glacial maximum, inferred from insect fossils from a tephra-buried soil at Tempest Lake, Seward Peninsula, Alaska. Palaeogeogr Palaeoclim Palaeoecol 267:245–255

    Article  Google Scholar 

  • Lambeck K, Chappell J (2001) Sea level change through the last glacial cycle. Science 292:679–686. doi:10.1126/science.1059549

    Article  Google Scholar 

  • Lindroth CH (1963) The ground beetles of Canada and Alaska, part 3. Opuscula Entomol Suppl 24:201–408

    Google Scholar 

  • Lindroth CH (1966) The ground beetles of Canada and Alaska, part 4. Opuscula Entomol Suppl 29:409–648

    Google Scholar 

  • Lozhkin AV, Anderson PM (1995) The last interglaciation in northeast Siberia. Quat Res 43:147–158

    Article  Google Scholar 

  • Lozhkin AV, Anderson PM, Matrosova TV, Minyuk PS (2007) The pollen record from El’gygytgyn lake: implications for vegetation and climate histories of northern Chukotka since the late middle Pleistocene. J Paleolimnol 37:135–153

    Article  Google Scholar 

  • Mann DH, Groves P, Reanier RE, Kunz ML (2010) Floodplains, permafrost, cottonwood trees, and peat: what happened the last time climate warmed suddenly in Arctic Alaska? Quat Sci Rev 29:3,812–3,830

    Article  Google Scholar 

  • Martinson DG, Pisia NG, Hays JD, Imbrie J, Moore TC, Shackleton NJ (1987) Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy. Quat Res 27:1–29

    Article  Google Scholar 

  • Matthews JV Jr (1983) A method for comparison of northern fossil insect assemblages. Geogr Phys Quat 37:297–306

    Google Scholar 

  • Matthews JV, Schweger CE, Janssens JA (1990) The last (Koy-Yukon) interglaciation in the northern Yukon evidence from unit 4 at Ch’ijee’s Bluff, Bluefish Basin. Geogr Phys Quat 44:341–362

    Google Scholar 

  • McAndrews JH, Berti AA, Norris G (1973) Key to the Quaternary pollen and spores of the great lakes region. Royal Ontario Museum, Toronto

    Google Scholar 

  • McDowell PF, Edwards ME (2001) Evidence of Quaternary climatic variations in a sequence of loess and related deposits at Birch Creek, Alaska: implications of the stage 5 climatic chronology. Quat Sci Rev 20:63–76

    Article  Google Scholar 

  • Miller GH, Brigham-Grette J, Alley RB, Anderson L, Anderson L, Bauch HA, Douglas MSV, Edwards ME, Elias SA, Finney BP, Fitzpatrick JJ, Funder SV, Herbert TD, Hinzman LD, Kaufman DS, MacDonald GM, Polyak L, Robock A, Serreze MC, Smol JP, Spielhagen R, White JCW, Wolfe AP, Wolff EW (2010) Temperature and precipitation history of the Arctic. Quat Sci Rev 29:1,679–1,715

    Article  Google Scholar 

  • Moore PD, Webb JA, Collinson ME (1991) Pollen analysis. Blackwell Scientific Publications, Oxford

    Google Scholar 

  • Muhs DR, Ager TA, Bettis EA, McGeehin J, Been JM, Begét JE, Pavich MJ, Stafford TWJ, Stevens DSP (2003) Stratigraphy and palaeoclimatic significance of late Quaternary loess-palaeosol sequences of the last interglacial-glacial cycle in central Alaska. Quat Sci Rev 22:1,947–1,986

    Article  Google Scholar 

  • Muhs DR, Pandolfi JM, Simmons KR, Schumann RR (2012) Sea-level history of past interglacial periods from uranium-series dating of corals, Curaçao, Leeward Antilles islands. Quat Res 78:157–169. doi:10.1016/j.yqres.2012.05.008

    Article  Google Scholar 

  • National Oceanic and Atmospheric Administration (2002) Monthly station normals of temperature, precipitation, and heating and cooling degree days 1971–2000. Climatography of the United States, No. 81. US. Department of Commerce

  • Nielsen MG (1987) The ant fauna (Hymenoptera: Formicidae) in northern and interior Alaska. A survey along the Trans-Alaskan Pipeline and a few highways. Entomol News 98:74–88

    Google Scholar 

  • Overpeck JT, Otto-Bleisner BL, Miller GH, Muhs DR, Alley RB, Kiehl JT (2006) Paleoclimatic evidence for future ice-sheet instability and rapid sea-level rise. Science 311:1,747–1,750. doi:10.1126/science.1115159

    Article  Google Scholar 

  • Péwé TL, Berger GW, Westgate JA, Brown PM, Leavitt SW (1997) Eva interglaciation forest bed, unglaciated East-Central Alaska: global warming 125,000 years ago. Geological society of America special paper 319. Geological society of America, Boulder, Colorado

  • Péwé TL, Westgate JA, Preece SJ, Brown PM, Leavitt SW (2009) Late Pliocene Dawson cut forest bed and new tephrochronological findings in the gold hill loess, east-central Alaska. Bull Geol Soc Am 121:294–320. doi:10.1130/B26323.1

    Google Scholar 

  • Preece SJ, Westgate JA, Stemper BA, Péwé TL (1999) Tephrochronology of late Cenozoic loess at Fairbanks, central Alaska. Bull Geol Soc Am 111:71–90

    Article  Google Scholar 

  • Preece SJ, Pearce NJG, Westgate JA, Froese DG, Jensen BJL, Perkins WT (2011) Old Crow tephra across eastern Beringia; a single cataclysmic eruption at the close of marine isotope stage 6. Quat Sci Rev 30:2,069–2,090. doi:10.1016/j.quascirev.2010.04.020

    Article  Google Scholar 

  • Reyes AV, Jensen BJ, Zazula GD, Ager TA, Kuzmina S, La Farge C, Froese DG (2010) A late-middle Pleistocene (marine isotope stage 6) vegetated surface buried by Old Crow tephra at the palisades, interior Alaska. Quat Sci Rev 29:801–811

    Article  Google Scholar 

  • Risebrobakken B, Balbon E, Dokken T, Jansen E, Kissel C, Labeyrie L, Richter T, Senneset L (2006) The penultimate deglaciation: high-resolution paleoceanographic evidence from a north–south transect along the eastern Nordic Seas. Earth Planet Sci Lett 241:505–516. doi:10.1016/j.epsl.2005.11.032

    Article  Google Scholar 

  • Santamaria L (2002) Why are most aquatic plants widely distibuted? Dispersal, clonal growth and small-scale herogeneity in a stressful environment. Acta Oecol 23:137–154

    Article  Google Scholar 

  • Schweger CE, Matthews JV (1985) Early and middle Wisconsinan environments of eastern Beringia stratigraphic and paleoecological implications of the Old Crow tephra. Geogr Phys Quat 34:275–290

    Google Scholar 

  • Schweger CE, Matthews JV (1991) The last (Koy-Yukon) interglaciation in the Yukon: comparisons with holocene and interstadial pollen records. Quat Int 10–12:85–94

    Article  Google Scholar 

  • Sculthorpe CD (1967) The biology of aquatic vascular plants. St. Martin’s Press, New York

    Google Scholar 

  • Seidenkrantz M-S, Bornmalm L, Johnsen SJ, Knudsen KL, Kuijpers A, Lauritzen S-E, Leroy SAG, Mergeal I, Schweger C, Van Vliet-Lanoë B (1996) Two-step deglaciation at the oxygen isotope stage 6/5e transition: the Zeifen-Kattegat climate oscillation. Quat Sci Rev 15:63–75

    Article  Google Scholar 

  • Shackleton J (1982) Paleoenvironmental histories from whitefish and Imuruk lakes, Seward Peninsula, Alaska. Institute of polar studies report. Institute of Polar Studies, Ohio State University, Columbus

    Google Scholar 

  • Shackleton NJ, Opdyke ND (1973) Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238: oxygen isotope temperatures and ice volumes on a 105 and 106 year scale. Quat Res 3:39–55

    Article  Google Scholar 

  • Smetana A (1985) Revision of the subfamily Helophorinae of the Nearctic region (coleoptera: hydrophilidae). Mem Entomol Soc Can No. 131

  • Tarasov P, Granoszewski W, Bezrukova E, Brewer S, Nita M, Abzaeva A, Oberhansli H (2005) Quantitative reconstruction of the last interglacial vegetation and climate based on the pollen record from lake Baikal, Russia. Clim Dynam 25:625–637. doi:10.1007/s00382-005-0045-0

    Article  Google Scholar 

  • Thompson RS, Anderson KH, Bartlein PJ (1999a) Atlas of relations between climatic parameters and distribution of important trees and shrubs in North America–Hardwoods. U.S. Geological survey professional paper 1650-B. US Department of the Interior, Washington

  • Thompson RS, Anderson KH, Bartlein PJ (1999b) Atlas of relations between climatic parameters and distribution of important trees and shrubs in North America–introduction and conifers. U.S. Geological survey professional paper 1650-A. U.S. Department of the Interior, Washington

  • Turner DG, Ward BC, Bond JD, Jensen BJL, Froese DG, Telka AM, Zazula GD, Bigelow NH (2013) Middle to late Pleistocene ice extents, tephrochronology and paleoenvironments of the white river area, southwest Yukon. Quat Sci Rev 75:59–77. doi:10.1016/j.quascirev.2013.05.011

    Article  Google Scholar 

  • van Nieuwenhove N, Bauch HA, Eynaud F, Kandiano E, Cortijo E, Turon J-L (2011) Evidence for delayed poleward expansion of North Atlantic surface waters during the last interglacial (MIS 5e). Quat Sci Rev 30:934–946. doi:10.1016/j.quascirev.2011.01.013

    Article  Google Scholar 

  • Viereck LA (1983) The effects of fire in black spruce ecosystems of Alaska and northern Canada. In: Wein RW, MacLean DA (eds) The role of fire in Northern circumpolar ecosystems. Wiley, Chichester, pp 201–220

    Google Scholar 

  • Waythomas CF, Lea PD, Walter RC (1993) Stratigraphic context of the Old Crow tephra, Holitna lowland, interior southwest Alaska. Quat Res 40:20–29

    Article  Google Scholar 

  • Weng C, Jackson ST (2000) Species differentiation of North American spruce (Picea) based on morphological and anatomical characteristics of needles. Can J Bot 78:1,367–1,383

    Google Scholar 

  • Werner RA, Holsten EH (1984) Scolytidae associated with felled white spruce in Alaska. Can Entomol 116:465–471

    Article  Google Scholar 

  • Western Regional Climate Center (2006) Fort Yukon monthly average temperature 1938–1990. http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?akfory. Accessed Sep 2013

  • Westgate JA (1989) Isothermal plateau fission-track ages of hydrated glass shards from silicic tephra beds. Earth Planet Sci Lett 95:226–234

    Article  Google Scholar 

  • Westgate JA, Walter RC, Pearce GW, Gorton MP (1985) Distribution, stratigraphy, petrochemistry, and palaeomagnetism of the late Pleistocene Old Crow tephra in Alaska and the Yukon. Can J Earth Sci 22:893–906

    Article  Google Scholar 

  • Zagwijn WH (1996) An analysis of Eemian climate in Western and Central Europe. Quat Sci Rev 15:451–469. doi:10.1016/0277-3791(96)00011-X

    Article  Google Scholar 

  • Zimmerman JR (1981) A revision of colymbetes of North America (Dytiscidae). Coleopt Bull 35:1–51

    Google Scholar 

Download references

Acknowledgments

The macrofossil results presented here would not have been possible without Hilary Birks’ training of NHB in plant macrofossil identification. NHB spent a very enjoyable postdoctoral year in Bergen where she wallowed in plant debris and soaked up all palaeoecological things. This work was funded by National Science Foundation grant OPP-0002362 to SAE, TDH, and MEE. Glen Berger participated in the field work and was a key member of our team. His untimely death occurred before his final TL ages were available for this paper. We also thank Cary Mock for a helpful discussion of MIS 5 palaeoclimates. Dan Mann assisted in the fieldwork at Birch Creek. We also thank two anonymous reviewers for their insightful comments which greatly improved this paper.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Nancy H. Bigelow.

Additional information

Communicated by A.E. Bjune.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Supplementary material 1 (PDF 19 kb)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Bigelow, N.H., Edwards, M.E., Elias, S.A. et al. Tundra and boreal forest of interior Alaska during terminal MIS 6 and MIS 5e. Veget Hist Archaeobot 23, 177–193 (2014). https://doi.org/10.1007/s00334-013-0425-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00334-013-0425-z

Keywords

Navigation