New paleontological and stratigraphical data on the upper - cretaceous transgression of the Pelagonian zone s.l. (Marmeiko, Ptoon Mt. NE Beotia)

Α. Μερμιγκη, Α. Μαρκοπουλου Διακαντωνη, Α. Ζαμπετακη Λεκκα
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Abstract

This paper concerns the study of a transgressive series, which overlies the upperjurassic oolitic limestones of subpelagonian zone, as well as the lateritic deposits, resulting from the alteration of the ophiolitic and fill the karstic cavities of the above mentioned limestones in NE Beotia (Fig.l). The purpose of this study is to• elucidate the age of the transgression, that occurred on the Jurassic limestones of the pelagonian platform at this region.• Discuss about the observed diachronism of the Late Cretaceous transgression on the Pelagonian platform.It is based on the study of micro- and macrofauna occurred in a section we describe in the "Marmeiko" area, on the Ptoon mountain. NOETH (1931) was the first who defined as Upper Turonian the age of the transgressive series, based on the study of Rudists. Later, BIGNOT & GUERNET (1968) studied the microfauna and attributed an age of lower Senonian. STEUBER (1993) based on the study of Hippuritidae, defined as Turonian and later (1995) as Turonian - Coniacian the age of the transgessive series. The basal part of the series consists of marls and marly limestones alternations. An abundant micro and macrofauna is found in this part of the section, as well as the first Rudist biostrome. In the middle part of the section 2 Rudist biostroms alternate with bioclastic limestones, containing abundant microfauna. In the upper part marls alternate with cherty limestones. The determinated micro- and macrofauna (Fig. 1), precises the age of the transgressive series as Santonian. This result confirms the diachronism of the transgressive phenomenon on the Pelagonian Upper- Jurassic limestones and the overthrusted ophiolites (AUBOUIN et al. 1960, BRUNN et al. 1972, KALLERGIS & ALBANTAKIS 1970, MAVRIDIS et al. 1979, NOETH 1931, BIGNOT & GUERNET 1968, CLEMENT & FERRIERE 1973, BIGNOT et al. 1973, STEUBER 1993, 1995, SKARPELIS & ZAMBETAKIS – LEKKAS 1998)
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Pelagonian带s.l. (Marmeiko, panton Mt. NE Beotia)上白垩统海侵的古生物和地层新资料
本文研究了东北贝奥提亚地区上侏罗统下拉哥尼亚带鲕状灰岩上覆的一套海侵系列,以及蛇绿岩蚀变后充填上述灰岩岩溶洞的红土矿床(图1)。本研究的目的是阐明发生在该地区巴拉哥尼亚台地侏罗纪灰岩上的海侵年龄。•讨论了在Pelagonian台地观测到的晚白垩世海侵历时。它是基于我们在普顿山“Marmeiko”地区描述的一段中发生的微型和大型动物群的研究。NOETH(1931)在对Rudists的研究基础上,首次将海侵系的时代定义为上Turonian。后来,BIGNOT & GUERNET(1968)对微动物群进行了研究,认为其时代为下塞涅世。STEUBER(1993)基于对河马科的研究,将其定义为Turonian,后来(1995)将其定义为Turonian - Coniacian的越海系列。该系列的基底部分由泥灰岩和泥灰岩相间组成。在该剖面的这一部分发现了丰富的微型和大型动物群,以及第一个鲁德生物层。在第二段中部,鲁德生物层与生物碎屑灰岩交替存在,含有丰富的微动物群。上部泥灰岩与砂质灰岩相间。经测定的微、大型动物群(图1),确定海侵系的年龄为三东期。这一结果证实了Pelagonian上侏罗统灰岩和逆冲蛇绿岩的海侵现象的历时性(AUBOUIN等人1960,BRUNN等人1972,KALLERGIS & ALBANTAKIS 1970, MAVRIDIS等人1979,NOETH 1931, BIGNOT & GUERNET 1968, CLEMENT & FERRIERE 1973, BIGNOT等人1973,STEUBER 1993, 1995, SKARPELIS & ZAMBETAKIS - LEKKAS 1998)。
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