O eustatyce, tektonice i innych zdarzeniach w późnym dewonie Gór Świętokrzyskich
Abstract
ON EUSTASY, TECTONICS AND OTHER EVENTS IN THE LATE DEVONIAN OF HOLY CROSS MTS
Summary
The methodological setting is outlined for the controversy between M. Narkiewicz (23) and M. Szulczewski (41), with special emphasis on constraints of the zonal biostratigraphy, a growing importable of process-oriented event and sequential stratigraphy and extensive significances of eustasy for carbonate ecosystems. The relationships between global eustatic fluctuations and local epeirogeny remain still crudely established in the Upper Devonian sedimentary record of the Holy Cross Mts; however, the dominating control of the first factor is in better agreement with evidences available, and with current approaches and results (8). As possible partial exception is indicated a controversial shallowing event in the Early gigas Chrone. The need of an integrated approach to the problems, particularly in the context of the latest Frasnian extinction, is obvious.
Summary
The methodological setting is outlined for the controversy between M. Narkiewicz (23) and M. Szulczewski (41), with special emphasis on constraints of the zonal biostratigraphy, a growing importable of process-oriented event and sequential stratigraphy and extensive significances of eustasy for carbonate ecosystems. The relationships between global eustatic fluctuations and local epeirogeny remain still crudely established in the Upper Devonian sedimentary record of the Holy Cross Mts; however, the dominating control of the first factor is in better agreement with evidences available, and with current approaches and results (8). As possible partial exception is indicated a controversial shallowing event in the Early gigas Chrone. The need of an integrated approach to the problems, particularly in the context of the latest Frasnian extinction, is obvious.