Hostname: page-component-cd9895bd7-mkpzs Total loading time: 0 Render date: 2024-12-27T08:19:54.033Z Has data issue: false hasContentIssue false

Dynamic early Holocene vegetation development on the Faroe Islands inferred from high-resolution plant macrofossil and pollen data

Published online by Cambridge University Press:  20 January 2017

Gina E. Hannon*
Affiliation:
Department of Geography, Roxby Building Liverpool L69 7ZT, England
Mats Rundgren
Affiliation:
Department of Geology, Quaternary Sciences, Lund University, S"lvegatan 12, SE-22362, Lund, Sweden
Catherine A. Jessen
Affiliation:
Department of Quaternary Geology, Geological Survey of Denmark and Greenland, "ster Voldgade 10, DK-1350 Copenhagen K, Denmark
*
*Corresponding author. Fax: +44 1517942866.E-mail address:Gina.Hannon@liv.ac.uk (G.E. Hannon).

Abstract

Vegetation dynamics during the earliest part of the Holocene (11,250"10,250"cal yr BP) have been reconstructed from a lacustrine sequence on Sandoy, the Faroe Islands, using detailed plant macrofossil and pollen evidence. The plant macrofossils suggest the initial vegetation was sparse herb and shrub tundra, with Salix herbacea and open-ground species, followed by the development of a denser and more species-rich arctic heathland after 11,150"cal yr BP. Despite high pollen values for Betula nana, macrofossils are rare. The bulk of the macrofossils recorded are S. herbacea and Empetrum leaves with numerous herb taxa and an abundance of Racomitrium moss. Conditions start to change around 10,800"cal yr BP, with increased catchment erosion and sediment delivery to the lake from ca. 10,600"cal yr BP, and a transition to alternating Cyperaceae and Poaceae communities between ca. 10,450 and 10,250"cal yr BP. This vegetation change, which has been recorded throughout the Faroes, has previously been interpreted as a retrogressive shift from woody shrubs to a herbaceous community. The detailed plant macrofossil data show the shift is the replacement of an Empetrum arctic heathland by grassland and moist sedge communities. These taxa dominate the modern landscape.

Type
Original Articles
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Andersen, S.T., (1980). Early and Late Weichselian chronology and birch assemblages in Denmark. Boreas 9, 5369.Google Scholar
Andresen, C.S., Bj"rck, S., Jessen, C., Rundgren, M., (2007). Early Holocene terrestrial climatic variability along a North Atlantic island transect: paleoceanographic implications. Quaternary Science Reviews 26, 19891998.Google Scholar
Bakke, J., Dahl, S.O., Nesje, A., (2005). Lateglacial and early Holocene palaeoclimatic reconstruction based on glacier fluctuations and equilibrium-line altitudes at northern Folgefonna, Hardanger, western Norway. Journal of Quaternary Science 20, 179198.Google Scholar
Bell, J.N.B., Tallis, J.H., (1973). Biological Flora of the British Isles, Empetrum nigrum L. Journal of Ecology 61, 289305.Google Scholar
Berger, A., Loutre, M.F., (1991). Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297317.Google Scholar
Berglund, B.E., Ralska-Jasiewiczowa, M., (1986). Pollen analysis and pollen diagrams. Berglund, B.E., Handbook of Holocene palaeoecolgy and palaeohydrology. John Wiley, Chichester., 455484.Google Scholar
Bertsch, K., (1941). Fr"chte und Samen. Ein Bestimmungsbuch zur Pflanzenkunde der vorgeschichtlichen Zeit. Handb"cher der praktischen Vorgeschichtsforschung, B and 1, Tafeln IV. Ferdinand Enke, Stuttgart, , Germany. Google Scholar
Birks, H.H., (1993). The importance of plant macrofossils in late-glacial climatic reconstructions: an example from western Norway. Quaternary Science Reviews 12, 719726.CrossRefGoogle Scholar
Birks, H.H., Ammann, B., (2000). Two terrestrial records of rapid climatic change during the glacial-Holocene transition (14,000-9,000 calendar years B.P.) from Europe. Proceedings of the National Academy of Sciences 97, 13901394.CrossRefGoogle ScholarPubMed
Bj"rck, S., Rundgren, M., Ingolfsson, O., Funder, S., (1997). The Preboreal oscillation around the Nordic Seas: terrestrial and lacustrine responses. Journal of Quaternary Science 12, 455465.3.0.CO;2-S>CrossRefGoogle Scholar
Bj"rck, S., Muscheler, R., Kromer, B., Andresen, C.S., Heinemeier, J., Johnsen, S.J., Conley, D., Koc, N., Spurk, M., Veski, S., (2001). High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger. Geology 29, 11071110.Google Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P.,, de Menocal, P., Priore, P., Cullen, H., Hajdas, I., Bonani, G., (1997). A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, 1257 536"1266.Google Scholar
Bronk Ramsey, C., (1995). Radiocarbon calibration and analysis of stratigraphy: The OxCal Program. Radiocarbon 37, 425"430.Google Scholar
Bronk Ramsey, C., (2001). Development of the radiocarbon program OxCal. Radiocarbon 43, 355363.Google Scholar
B"cher, T.W., (1937). Nogle studier over Faer"ernes alpine vegetation. Botanisk Tidskrift 44, 154201.Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammer, C.U., Hvidberg, C.S., Steffensen, J.P., Sveinbj"rnsdottir, A.E., Jouzel, J., Bond, G., (1993). Evidence for general instability of past climate from a 250-kyr ice-core record. Nature 364, 218220.Google Scholar
Davis, M., Brubacker, L.B., Webb III, T., (1973). Calibration of absolute pollen influx. Birks, H.J.B., West, R.G., Quaternary Plant Ecology. Blackwell, Oxford., 925.Google Scholar
Fisher, T.G., Smith, D.G., Andrews, J.T., (2002). Preboreal oscillation caused by a glacial Lake Agassiz flood. Quaternary Science Reviews 21, 873878.Google Scholar
Fosaa, A., (2001). A review of plant communities of the Faroe Islands. Fr""skaparrit 48, 4154.Google Scholar
Fossitt, J.A., (1996). Late Quaternary vegetation history of the Western Isles of Scotland. New Phytologist 132, 171196.Google Scholar
Fredskild, B., (1967). Palaeobotanical investigations at Sermermiut, Jakobshavn, West Greenland. Meddelelser om Gr"nland 178, 154.Google Scholar
Gorczynski, W., (1920). Sur le calcul du degre du continentalisme et son application dans la climatologie. Geografiska Annaler 2, 324331.Google Scholar
Hald, M., Hagen, S., (1998). Early Preboreal cooling in the Nordic Seas region triggered by meltwater. Geology 26, 615618.2.3.CO;2>CrossRefGoogle Scholar
Hannon, G.E., Gaillard, M.-J., (1997). The plant-macrofossil record of past lake-level changes. Journal of Paleolimnology 18, 1528.Google Scholar
Hannon, G., Bradshaw, R.H.W., (2008). Human impact and landscape change at Argisbrekka. In: Mahler, D.L., (Ed.), S"teren ved Argisbrekka . Economic development during the Viking Age and Early Middle Ages on the Faroe Islands. Annales Societatis Scientiarum F"roensis Supplemtentum 47. Faroe University Press. T"rshavn, , Faroe Islands., pp. 306"321.Google Scholar
Hannon, G.E., Wasteg"rd, S., Bradshaw, E., Bradshaw, R.H.W., (2001). Human impact and landscape degradation on the Faroe Islands. Proceedings of the Royal Irish Academy 101B, 129139.Google Scholar
Hannon, G.E., Bradshaw, R.H.W., Wasteg"rd, S., (2003). Rapid vegetation change during the early Holocene in the Faroe Islands detected in terrestrial and aquatic ecosystems. Journal of Quaternary Science 18, 615619.Google Scholar
Hannon, G.E., Bradshaw, R.H.W., Bradshaw, E.G., Snowball, I., Wasteg"rd, S., (2005). Climate change and human settlement as drivers of late-Holocene vegetational change on the Faroe Islands. The Holocene 15, 639647.Google Scholar
Hansen, K., (1966). Vascular Plants in the Faeroes. Horizontal and Vertical Distribution. Dansk Botanisk Arkiv 24. Dansk Botanisk Forening, Copenhagen K, Denmark.Google Scholar
Isarin, R.F.B., Bohncke, S.J.P., (1999). Mean July temperatures during the Younger Dryas in Northwestern and Central Europe as inferred from climate indicator plant species. Quaternary Research 51, 158173.CrossRefGoogle Scholar
Jessen, C.A., Rundgren, M., Bj"rck, S., Muscheler, R., (2007). Climate forced atmospheric CO2 variability in the early Holocene: a stomatal frequency reconstruction. Global and Planetary Change 57, 247260.CrossRefGoogle Scholar
Jessen, C.A., Rundgren, M., Bj"rck, S., Andresen, C.S., Conley, D., (2008). Variability and seasonality of North Atlantic climate during the early Holocene: evidence from Faroe Island lake sediments. The Holocene 18, 110.Google Scholar
J"hansen, J., (1985). Studies in the vegetational history of the Faroe and Shetland Islands. F"roya Fr""skaparfelag, T"rshavn. Faroe Islands. Google Scholar
Leivsson, T.G., (1989). Areas laid out for afforestation 1885"1985 in the Faroe Islands. H"jgaard, A., J"hansen, J., Odum, S., A Century of Tree-Planting in the Faroe Islands. F"roya Fr""skaparfelag,T"rshavn. 3550.Google Scholar
McVean, D.N., Ratcliffe, D.A., (1962). Plant communities of the Scottish Highlands. Monographs of the Nature Conservancy 1.Google Scholar
Moore, P.D., Webb, J.A., Collinson, M.E., (1991). Pollen analysis. Blackwell, Oxford. Google Scholar
Muscheler, R., Beer, J., Wagner, G., Finkel, R.C., (2000). Changes in deep-water formation during the Younger Dryas event inferred from 10Be and 14C records. Nature 408, 567570.Google Scholar
Oswald, W.W., Anderson, P.M., Brubaker, L.B., Hu, F.S., Engstrom, D.R., (2003). Representation of tundra vegetation by pollen in lake sediments of northern Alaska. Journal of Biogeography 30, 521535.CrossRefGoogle Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C.J. H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hogg, A.G., Hughen, K.A., Kromer, B., McCormac, G., Manning, S., Ramsey, C., Bronk, , Reimer, R.W., Remmele, S., Southon, J., Stuiver, M., Talamo, S., Taylor, F.W., Van der Plicht, J., Weyhenmeyer, C.E., (2004). IntCal04 terrestrial radiocarbon age calibration, 0-26 Cal Kyr BP. Radiocarbon 46, 10291058.Google Scholar
Rundgren, M., (1995). Biostratigraphic evidence of the Aller"d"Younger Dryas"Preboreal oscillation in northern Iceland. Quaternary Research 44, 405416.Google Scholar
Rundgren, M., (1998). Early-Holocene vegetation of northern Iceland: pollen and plant macrofossil evidence from the Skagi peninsula. The Holocene 8, 553"564.Google Scholar
Sepp", H., Nyman, M., Korhola, A., Weckstr"m, J., (2002). Changes of treelines and alpine vegetation in relation to post-glacial climate dynamics in northern Fennoscandia based on pollen and chironomid records. Journal of Quaternary Science 17, 287301.Google Scholar
Snowball, I., Korhola, A., Briffa, K., Ko", N., (2004). Holocene climate dynamics in Fennoscandia and the North Atlantic. Batterbee, R.W., Gasse, F., Stickley, C.E., Past Climate Variability through Europe and Africa 6, Springer, Dordrecht, The Netherlands., 465487.Google Scholar
S"gaard, H., (1996). Climate and weather. Guttesen, R., Atlas of Denmark Series II, Volume 5. The F"roe Islands Topographical Atlas. A. Reitzels Forlag for Det Kongelige Danske Geografiske Selskab and Kort og Matrikelstyrelsen, Copenhagen., 2427.Google Scholar
Teller, J.T., Leverington, D.W., Mann, J.D., (2002). Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation. Quaternary Science Reviews 21, 879887.Google Scholar
Wasteg"rd, S., Bj"rck, S., Grauert, M., Hannon, G., (2001). The Mjauv"tn tephra and other Holocene tephra horizons from the Faroe Islands: a link between the Icelandic source region, the Nordic Seas and the European continent. The Holocene 11, 101109.Google Scholar
Watts, W.A., (1978). Plant macrofossils and Quaternary Paleoecology. Walker, D., Guppy, J.C., Biology and Quaternary Environments. Australian Academy of Sciences, Canberra., 5367.Google Scholar
Whittington, G., Buckland, P., Edwards, K.J., Greenwood, M., Hall, A.M., Robinson, M., (2003). Multiproxy Devensian Late-glacial and Holocene environmental records at an Atlantic coastal site in Shetland. Journal of Quaternary Science 18, 151168.CrossRefGoogle Scholar
"orsteinsson, I., Arnalds, "., (1992). The vegetation and soils of the Thingvallavatn area. Oikos 64, 105116.Google Scholar