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The Late‐Quaternary vegetational history of Loch a'Bhogaidh, Rinns of Islay S.S.S.I., Scotland
Author(s) -
EDWARDS KEVIN J.,
BERRIDGE JAMES M. A.
Publication year - 1994
Publication title -
new phytologist
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.742
H-Index - 244
eISSN - 1469-8137
pISSN - 0028-646X
DOI - 10.1111/j.1469-8137.1994.tb04038.x
Subject(s) - holocene , stadial , pollen , alnus glutinosa , mesolithic , juniperus communis , juniper , quaternary , arboreal locomotion , peat , geography , ecology , geology , archaeology , physical geography , alder , forestry , paleontology , biology , habitat
summary Holocene and partial Lateglacial age percentage and concentration pollen diagrams are presented of two profiles from the Inner Hebridean site of Loch a'Bhogaidh, Islay. The Lateglacial deposits may extend back to Lateglacial Interstadial times and a relative lack of Juniperus communis pollen is noted. The early Holocene deposits contain abundant Betula and Corylus avellana ‐type pollen, followed by substantial amounts of pollen from other arboreal taxa, namely Pinus Sylvestris, I Ulmus, Quercus, Alnus glutinosa and Salix. There is pollen, charcoal and sedimentary evidence for possible Mesolithic age environmental impacts, and a hunter‐gatherer presence on Islay may date from the 10th millennium BP. Major woodland clearance dates from middle Bronze Age runes onwards ( c. 3610 BP) and involved a mixed farming regime. The later Holocene records show that soil deterioration was occurring as heath and acid grassland taxa become prominent. These events may have resulted from land use pressures or climate change.