Stratigraphic position of interglacial deposits at Przasnysz
Abstract
Geological situation of the interglacial series of Przasnysz has been presented with reference to the nearby comprehensively described profiles. Basing on these profiles the stratigraphy of Pleistocene deposits has been determined according to the results of litho-petrographic, mineralogic and palaeontologie investigations as well as TL datings. The sequence has been subdivided into five major glacial units (including bipartite ones) and four interglacials. It has been proved that the interglacial deposits at Przasnysz refer to the second interglacial period (after Podlasie Interglacial which is defined as the oldest one). However the results of palaeobotanic analysis (by K.Mamakowa) revealed the pattern of vegetation parallel to Mazovian Interglacial (Holstein) succession. The latter is the fourth (last) of the presented interglacials. K.Mamakowa proposed an attempt to correlation of Przasnysz Interglacial with the IVth Interglacial of the Cromerian complex in Holland.Downloads
Published
2013-04-08
Issue
Section
Articles
License
Authors who publish with this journal agree to the following terms:- Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as this can lead to productive exchanges and earlier and more frequent citation of the published work (See The Effect of Open Access).