Birch hybridization in Thistilfjördur, North-east Iceland during the Holocene

Past episodes of birch hybridization in Iceland were studied by pollen analysis. The low stature and polycormic form of downy birch Betula pubescens in the subarctic probably results from such hybridization with the dwarf birch Betula nana. Two previous studies in different regions in Iceland reveal...

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Bibliographic Details
Main Authors: Lilja Karlsdóttir 1952-, Margrét Hallsdóttir 1949-, Ólafur Eggertsson 1964-, Ægir Þór Þórsson 1970-, Kesara Margrét Jónsson 1951-
Other Authors: Landbúnaðarháskóli Íslands
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/1946/19878
Description
Summary:Past episodes of birch hybridization in Iceland were studied by pollen analysis. The low stature and polycormic form of downy birch Betula pubescens in the subarctic probably results from such hybridization with the dwarf birch Betula nana. Two previous studies in different regions in Iceland revealed events of hybridization connected to early B. pubescens expansion. The present study examined a peat monolith from Thistilfjördur, North-east Iceland, covering the last ten thousand years. Betula pollen was measured, proportions of B. nana and B. pubescens calculated and the presence of hybrids estimated. Betula pubescens expansion started around 7.2 cal ka BP with a peak in non-triporate pollen, indicating hybrids. Low Betula pollen concentrations followed. A second period of considerable hybridization is indicated around 3.3 cal ka BP. Both peaks were associated with B. pubescens expansion. Tegundablöndun ilmbjarkar og fjalldrapa var rannsökuð í frjókornum. Lágar og margstofna ilmbjarkir á norðlægum slóðum eru líklega afleiðing slíkrar blöndunar. Tvær eldri rannsóknir frá mismunandi landshlutum sýndu hrinur blöndunar snemma á Nútíma sem tengdust framrás ilmbjarkar. Í þessari rannsókn voru sýni tekin úr mósniði í Þistilfirði, sem spannar síðustu tíu þúsund ár. Birkifrjókorn voru mæld, hlutföll tegundanna reiknuð og leitað ummerkja um blöndunina. Ilmbjörk tók að breiðast út fyrir um 7200 árum og fram kom toppur afbrigðilegra frjókorna sem gefa til kynna fjölda blendingstrjáa. Tímabil með litlu birki fylgdi í kjölfarið en önnur hrina erfðablöndunar varð fyrir um 3300 árum. Báðar hrinurnar tengdust aukinni útbreiðslu ilmbjarkar.