Poziomy amonitowe oksfordu górnego w Jurze Częstochowskiej
Abstract
AMMONITE ZONES OF THE UPPER OXFORDIAN IN THE CZĘSTOCHOWA JURASSIC BELTSummaryThis raport presents the stratigraphy of the Upper Oxfordian deposits that occur between Częstochowa, Rębielice Królewskie and Zawady. The ammonite fauna found in these deposits represents the zone Perisphinctes cautisnigrae sensu lato and part of the zone Ringstaedia pseudocordata. An analysis of the Upper Jurassic fauna found in the Częstochowa Jurassic Belt shows that the deposits may be correlated with those of the same age in England (H. J. Callomon, 1964), France (R. Enay, 1966, 1967) and Germany (A. Zeiss, 1966). The uppermost zone of the Upper Oxfordian, i.e. the zone Idoceras planula has been distinguished by A. Wierzbowski (1965).The existing possibility of distinguishing ammonite zones in the Upper Oxfordian deposits denies any conclusion as to a necessity of distinguishing “a new stage”.Downloads
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).
