(Table 3) Pollen analytical and carpological record of the outcrop Hölle below Dwadieden Park, Rügen Island ...

Pollen analyses and 14C-datings were carried out on two late glacial profiles from Ruegen Island, Mecklenburg-Vorpommern at the southwestern Baltic coast. The palaeoclimatic and palaeoecologic interpretations were supported by carpological investigations. The organogenic deposits of the 'Hoelle...

Full description

Bibliographic Details
Main Authors: Strahl, Jaqueline, Keding, Elmar
Format: Dataset
Language:English
Published: PANGAEA 1996
Subjects:
Sample ID
Cliff height
Betula pubescens
Juniperus sp.
Salix sp.
Arctostaphylos uva-ursi
Betula nana
Bryophyta
Carex aquatilis
Carex spp.
Caryophyllaceae
Comarum palustre
Eleocharis palustris
Hippuris vulgaris
Linaria vulgaris
Menyanthes trifoliata
Polygonum sp.
Potentilla anserina
Selaginella selaginoides
Sparganium minimum
Thalictrum simplex
Typha sp.
Urtica dioica
Chara sp.
Groenlandia densa
Myriophyllum spicatum
Nitella sp.
Nymphaea sp.
Potamogeton cf. alpinus
Potamogeton cf. coloratus
Potamogeton filiformis
Potamogeton friesii
Potamogeton natans
Potamogeton cf. perfoliatus
Potamogeton perfoliatus
Potamogeton sp.
Ranunculus aquatilis
Cenococcum geophilum
Coleoptera
Cristatella mucedo
Daphina sp.
Reworked species
Sampling by hand
Abundance estimate
Groenlandia
Online Access:https://dx.doi.org/10.1594/pangaea.785420
https://doi.pangaea.de/10.1594/PANGAEA.785420
Description
Summary:Pollen analyses and 14C-datings were carried out on two late glacial profiles from Ruegen Island, Mecklenburg-Vorpommern at the southwestern Baltic coast. The palaeoclimatic and palaeoecologic interpretations were supported by carpological investigations. The organogenic deposits of the 'Hoelle' outcrop near Dwasieden Park were chosen because of their unique stratigraphic position, which according to PANZIG (1989), lay under a m3m-Glacial Till of the Mecklenburg Advance (W3). The results indicated that the initial phase of the late glacial sedimentation in a relatively small and asymmetrical lake basin (in comparison with the larger Nieder- and Credner lake to the southwest), probably had its origin in the older Alleroed (II a) after FIRBAS (1949).The basal clastic sediments were rapidly followed by peat deposits and later, due to a rising water table, by muds rich in organic matter. The area was covered with sparse Betula-(Pinus) forests having heliophilous late-glacial elements typical of the surrounding ... : Abundances as follows: R = einzeln/rare (1-2 ind.), F = einige/few, C = häufig/common, A = massenhaft/abundant (>100 ind.). ...

Similar Items