Mesozoic Biotas of Scandinavia and its Arctic Territories
Scandinavia and its Arctic territories of Svalbard and Greenland represent geographical regions with a long history of Mesozoic palaeontology. However, the last few decades have witnessed a surge of new discoveries. Especially famous are the Triassic and Late Jurassic Lagerstätten of East Greenland and Spitsbergen in the Svalbard Archipelago, together with the Late Cretaceous strata of southern Sweden and the UNESCO World Heritage locality at Stevns Klint in Denmark. The latter records one of the most complete terminal Mesozoic rock successions known globally. Collectively, these deposits encompass the spectrum of Mesozoic biotic evolution, including the explosive radiation of marine faunas after the Permian–Triassic extinction, seminal specialization of amniotes for life in the sea, Late Triassic–Jurassic domination of the land by dinosaurs and the Cretaceous development of modern terrestrial floras and marine ecosystems. This volume, authored by leading experts in the field, encapsulates key aspects of the latest research and will provide a benchmark for future investigations into the Scandinavian Mesozoic world.
Coprolites from the Late Triassic Kap Stewart Formation, Jameson Land, East Greenland: morphology, classification and prey inclusions
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Published:January 01, 2016
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CiteCitation
Bitten Bolvig Hansen, Jesper Milàn, Lars B. Clemmensen, Jan Schulz Adolfssen, Eliza Jarl Estrup, Nicole Klein, Octávio Mateus, Oliver Wings, 2016. "Coprolites from the Late Triassic Kap Stewart Formation, Jameson Land, East Greenland: morphology, classification and prey inclusions", Mesozoic Biotas of Scandinavia and its Arctic Territories, B. P. Kear, J. Lindgren, J. H. Hurum, J. Milàn, V. Vajda
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Abstract
A large collection of vertebrate coprolites from black lacustrine shales in the Late Triassic (Rhaetian–Sinemurian) Kap Stewart Formation, East Greenland is examined with regard to internal and external morphology, prey inclusions, and possible relationships to the contemporary vertebrate fauna. A number of the coprolites were mineralogically examined by X-ray diffraction (XRD), showing the primary mineral composition to be apatite, clay minerals, carbonates and, occasionally, quartz in the form of secondary mineral grains. The coprolite assemblage shows multiple sizes and morphotypes of coprolites, and different types of prey inclusions, demonstrating that the coprolite assemblage originates from a variety of different producers.
A description of the size, shape, structure, texture, contents and preservation of the 328 specimens is available at https://doi.org/10.6084/m9.figshare.c.2134335
- Arctic region
- assemblages
- biogenic structures
- burrows
- carnivorous taxa
- Chondrichthyes
- Chordata
- classification
- coprolites
- correlation
- depositional environment
- diet
- East Greenland
- Elasmobranchii
- feeding
- fossils
- fragments
- grains
- Greenland
- ichnofossils
- identification
- Jameson Land
- Jurassic
- lacustrine environment
- Lower Jurassic
- measurement
- Mesozoic
- mineral composition
- morphology
- morphometry
- nomenclature
- Pisces
- predation
- preservation
- sedimentary structures
- shape analysis
- size
- statistical distribution
- teeth
- textures
- Triassic
- Upper Triassic
- Vertebrata
- X-ray diffraction data
- Kap Stewart Formation
- Wood Bjerg Greenland