Leroy, Suzanne A. G. (2007): Progress in palynology of the Gelasian-Calabrian Stages in Europe; ten messages

Leg/Site/Hole:
ODP 108
ODP 108 658
Identifier:
2013-025977
georefid

10.1016/j.revmic.2006.08.001
doi

Creator:
Leroy, Suzanne A. G.
Brunel University, Department of Geography and Earth Sciences, Uxbridge, United Kingdom
author

Identification:
Progress in palynology of the Gelasian-Calabrian Stages in Europe; ten messages
2007
In: Bertini, Adele (prefacer), Climate and paleoenvironmental changes during the Quaternary; palynologic evidence
Elsevier, Paris, France
50
4
293-308
Europe has at present the most extensive network of palynological sites covering the Late Pliocene and the Early Pleistocene or roughly the Gelasian-Calabrian Stages. This paper covers 10 points of recent progress in the palynology of this time period: 1) the contribution of palynology to truly global stratigraphy, 2) the existence and steps of vegetation succession after a glacial period, 3) the causes for the disappearance from Europe of some taxa, 4) the location and the types of vegetation refugia, 5) the causes of the low arboreal pollen representation in glacial times, 6) the extent of extreme glacial conditions, 7) the input of long marine records to short terrestrial ones, 8-9) cyclopalynostratigraphy for wiggle matching dating and duration estimations and, finally, 10) short glacial periods and long interglacial ones in an obliquity-forced climate.
English
Coverage:Geographic coordinates:
North:39.0500
West:-18.3451East: 17.0700
South:20.4457

Stratigraphy; Paleobotany; Atlantic Ocean; biogeography; biostratigraphy; Calabria Italy; Calabrian; Cenozoic; Crotone Italy; cyclostratigraphy; DNA; Europe; Gelasian; glaciation; Italy; lacustrine environment; Leg 108; lower Pleistocene; marine environment; microfossils; miospores; Neogene; North Atlantic; nucleic acids; Ocean Drilling Program; ODP Site 658; paleoclimatology; paleoenvironment; palynomorphs; Pleistocene; Pliocene; pollen; Quaternary; refugia; Southern Europe; stratotypes; Tertiary; upper Pliocene; vegetation;

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