Indicator value of oribatid mites in determining past permafrost dynamics in northern European sub-Arctic peatlands

Author:

Markkula Inkeri1ORCID,Oksanen Pirita2,Kuhry Peter3

Affiliation:

1. Biodiversity Unit; Zoological Museum; University of Turku; Turku FIN-20014 Finland

2. Bladintie 44-46 A 4; Kaskinen 64260 Finland

3. Department of Physical Geography; Stockholm University; Stockholm SE-10691 Sweden

Funder

Suomen Kulttuurirahasto

Lapin Rahasto

Oskar Öflunds Stiftelse

Maj ja Tor Nesslingin Säätiö

Fourth Framework Programme

FIGARE Program of the Academy of Finland (ARCTICA project)

Sixth Framework Programme

Vetenskapsrådet

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Reference79 articles.

1. Elemental and isotopic carbon and nitrogen records of organic matter accumulation in a Holocene permafrost peat sequence in the East European Russian Arctic;Andersson;Journal of Quaternary Geology,2012

2. Palaeoecology of a palsa and a filled thermokarst pond in a permafrost peatland, subarctic Quebec, Canada;Arlen-Bouliot;The Holocene,2005

3. Holocene palaeoclimates from peat stratigraphy: macrofossil proxy climate records from three oceanic raised bogs in England and Ireland;Barber;Quaternary Science Reviews,2003

4. Oribatid mite biodiversity in agroecosystems: role for bioindication;Behan-Pelletier;Agriculture Ecosystems and Environment,1999

5. Oribatida of Canadian peatlands;Behan-Pelletier;Memoirs of Entomological Society of Canada,1994

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