Trace fossils and depositional environments of the middle Turonian sandstones  in the Upper Nysa Kłodzka Graben (Sudetes, Poland) revisited

Chrząstek, Alina; Nowicka, Nadia

doi:10.7306/gq.1578

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2024

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Cited by 3 publications

References 96 publications

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Body fossil assemblages from the Lower Idzików Beds (Coniacian) in the Upper Nysa Kłodzka Graben, south-west Poland: Preliminary taphonomic, palaeoecological and palaeogeographical data

Chrząstek,

Jagt-Yazykova,

Jagt

2024

Cretaceous Research

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Body fossil assemblages from the Lower Idzików Beds (Coniacian) in the Upper Nysa Kłodzka Graben, south-west Poland: Preliminary taphonomic, palaeoecological and palaeogeographical data

Chrząstek,

Jagt-Yazykova,

Jagt

2024

Cretaceous Research

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Significance of the trace fossil Macaronichnus from the Cenomanian low-latitude nearshore deposits of the Saharan Atlas, Algeria

Naimi,

Mahboubi,

Vinn

et al. 2024

Proceedings of the Geologists' Association

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A First Report of the Ichnogenus <em>curvolithus</em> From the Mojado Formation, Cerro De Cristo Rey, Sunland Park, New Mexico.

Sanchez

Kappus

2022

New Mexico Geological Society, 2022 Annual Spring Meeting, Proceedings Volume, Theme: "Karst in New Mexico in Recognition of 20

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As part of a continuing investigation of trace fossils from the lower-most, Albian Sarten Member of the Mojado Formation, we report the first description of Curvolithus simplex at Cerro de Cristo Rey, Sunland Park, New Mexico. C.simplex is a horizontal, three-lobed trace interpreted as a repichnia. Other traces in this ichnoassemblage that are commonly associated with the Cruziana ichnofacies include Thalassinoides, Arthrophycus, Planolities, scratch marks (and others not yet reported). Our Curvolithus specimensare preserved exclusively in convex epirelief on iron-stained, massive sandstones, interbedded with thin grey shales. At this location the lower contact of the Sarten Member is easily distinguishable from the Mesilla Valley Formation below. Although the base of the Mojado Formation was originally defined arbitrarily by the thickness of sandstone interbeds, or a change in sandstone lithology, we see a distinct change in ichnoassemblages between these two Formations, which may be used to define the contact in the future.

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Trace fossils and depositional environments of the middle Turonian sandstones in the Upper Nysa Kłodzka Graben (Sudetes, Poland) revisited

Abstract: Trace fos sils and depositional en vi ron ments of the mid dle Turonian sand stones in the Upper Nysa K³odzka Graben (Sudetes, Po land) re vis ited. Geo log i cal Quar terly, 65: 10,

Cited by 3 publications

References 96 publications

Body fossil assemblages from the Lower Idzików Beds (Coniacian) in the Upper Nysa Kłodzka Graben, south-west Poland: Preliminary taphonomic, palaeoecological and palaeogeographical data

Body fossil assemblages from the Lower Idzików Beds (Coniacian) in the Upper Nysa Kłodzka Graben, south-west Poland: Preliminary taphonomic, palaeoecological and palaeogeographical data

Significance of the trace fossil Macaronichnus from the Cenomanian low-latitude nearshore deposits of the Saharan Atlas, Algeria

A First Report of the Ichnogenus <em>curvolithus</em> From the Mojado Formation, Cerro De Cristo Rey, Sunland Park, New Mexico.

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