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・ Hagens
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・ Hagenthal-le-Haut
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Hagbard Jonassen
・ Hagbard's gallow
・ Hagbart Haakonsen
・ Hagbart Steffens
・ Hagbarth Dahlmann
・ Hagbarth Schjøtt, Jr.
・ Hagbarth Schjøtt, Sr.
・ Hagberg
・ Hagberg (Welzheim Forest)
・ Hagbo
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・ Hagby Runestones
・ Hagbyhöjden
・ Hagbyån
・ Hagdale Chromate Railway


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Hagbard Jonassen : ウィキペディア英語版
Hagbard Jonassen
Hagbard Jonassen (1903–1977) was a Danish botanist, quaternary geologist, war resister and nuclear disarmament proponent. He made a lasting impact on the interpretation of pollen diagrams, including the use of modern pollen deposition in moss polsters to aid interpretation and the consideration of pollen productivity in different types of vegetation.
== Professional life ==
He studied natural history at the University of Copenhagen and obtained his M.Sc. (cand. mag.) in 1931. He then became an assistant to Knud Jessen, who was the professor of botany at the University of Copenhagen and director of the Copenhagen Botanical Garden and one of the pioneers of pollen analysis in quaternary geology. He assisted Jessen in his work on Irish vegetation history.
Jonassen’s list of papers is short. Nevertheless, his doctoral dissertation from 1950 had a lasting impact on its field in two respects. Jonassen pioneered the use pollen collected from moss polsters to assess the modern pollen rain and, by comparison with the species composition of surrounding vegetation, he was able to infer past vegetation from fossil pollen spectra much more accurately than before. Hence, he concluded that 1) cultivated crops such as cereals (except rye), beet, clover and lucerne had very low pollen production and the pollen signal from such areas would have a much higher detection limit than more productive types of land. Similarly, the pollen signal from un-wooded terrain like heathland and grassland could be completely swamped in pollen production from wind-pollinated trees. 2) Pollen dispersal in forest very limited local due to restricted wind speed, which was later confirmed by detailed investigations by Henrik Tauber.
Jonassen’s work on the Holocene history of heathlands in Jutland showed that forest had preceded heathland. He hypothesized that climate change had led to abandonment of agriculture and heathland expansion. More recent investigations in Denmark and Norway have shown that heathland expansion was metachronous, i.e. occurring at multiple separate locations to different times, suggesting an overriding impact of humans and less of importance for climate change.

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