A detailed early postglacial (Flandrian) pollen diagram from Cwm Idwal, North Wales

Palynological investigation of lacustrine sediments in Llyn Idwal, in the uplands of Snowdonia, North Wales, has shown that pollen assemblages predating those at the base of Godwin's (1955) pollen diagram are recorded. These earlier pollen assemblages do not, however, indicate a revision of the...

Ausführliche Beschreibung

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1979. - 125(1993), 1 vom: 20. Sept., Seite 175-191
1. Verfasser: Tipping, Richard (VerfasserIn)
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 1993
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Early Flandrian Palynology Snowdonia climate change
LEADER 01000naa a22002652 4500
001 NLM324291973
003 DE-627
005 20231225190012.0
007 cr uuu---uuuuu
008 231225s1993 xx |||||o 00| ||eng c
024 7 |a 10.1111/j.1469-8137.1993.tb03875.x  |2 doi 
028 5 2 |a pubmed24n1080.xml 
035 |a (DE-627)NLM324291973 
035 |a (NLM)33874605 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Tipping, Richard  |e verfasserin  |4 aut 
245 1 2 |a A detailed early postglacial (Flandrian) pollen diagram from Cwm Idwal, North Wales 
264 1 |c 1993 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Revised 20.04.2021 
500 |a published: Print 
500 |a Citation Status PubMed-not-MEDLINE 
520 |a Palynological investigation of lacustrine sediments in Llyn Idwal, in the uplands of Snowdonia, North Wales, has shown that pollen assemblages predating those at the base of Godwin's (1955) pollen diagram are recorded. These earlier pollen assemblages do not, however, indicate a revision of the Loch Lomond Readvance age of the last glaciers to occupy the cwm, Arctic-alpine flora presently growing on the cliffs of Cwm Idwal colonized the catchment as pioneer communities in the earliest postglacial, immediately following ice decay, but appear to have been driven to their present niches very early in the postglacial. Their subsequent reappearance is explained by natural or anthropogenically induced instability in local woodland, or perhaps by increased erosion and stream How affecting pollen transport from cliffs. Evidence is presented of a brief period of arid climate during the expansion of Juniperus, at around 10000 BP 
650 4 |a Journal Article 
650 4 |a Early Flandrian 
650 4 |a Palynology 
650 4 |a Snowdonia 
650 4 |a climate change 
773 0 8 |i Enthalten in  |t The New phytologist  |d 1979  |g 125(1993), 1 vom: 20. Sept., Seite 175-191  |w (DE-627)NLM09818248X  |x 1469-8137  |7 nnns 
773 1 8 |g volume:125  |g year:1993  |g number:1  |g day:20  |g month:09  |g pages:175-191 
856 4 0 |u http://dx.doi.org/10.1111/j.1469-8137.1993.tb03875.x  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 125  |j 1993  |e 1  |b 20  |c 09  |h 175-191