University of Leicester
Browse
Bennett et al 2016_Sedimentology_sandy siltstones_submitted revised MS.pdf (4.17 MB)

Early Mississippian sandy siltstones preserve rare vertebrate fossils in seasonal flooding episodes

Download (4.17 MB)
journal contribution
posted on 2017-08-29, 10:48 authored by Carys E. Bennett, Timothy I. Kearsey, Sarah J. Davies, David Millward, Jennifer A. Clack, Timothy R. Smithson, John E. A. Marshall
Flood-generated sandy siltstones are under-recognised deposits that preserve key vertebrate (actinopterygians, rhizodonts, and rarer lungfish, chondrichthyans and tetrapods), invertebrate and plant fossils. Recorded for the first time from the lower Mississippian Ballagan Formation of Scotland, more than 140 beds occur throughout a 490 m thick core succession characterised by fluvial sandstones, palaeosols, siltstones, dolostone ‘cementstones’ and gypsum from a coastal–alluvial plain setting. Sandy siltstones are described as a unique taphofacies of the Ballagan Formation (Scotland, UK); they are matrix-supported siltstones with millimetre-sized siltstone and very fine sandstone lithic clasts. Common bioclasts include plants and megaspores, fish, ostracods, eurypterids and bivalves. Fossils have a high degree of articulation compared with those found in other fossil-bearing deposits, such as conglomerate lags at the base of fluvial channel sandstones. Bed thickness and distribution varies throughout the formation, with no stratigraphic trend. The matrix sediment and clasts are sourced from the reworking of floodplain sediments including desiccated surfaces and palaeosols. Secondary pedogenic modification affects 30% of the sandy siltstone beds and most (71%) overlie palaeosols or desiccation cracks. Sandy siltstones are interpreted as cohesive debris flow deposits that originated by the overbank flooding of rivers and due to localised floodplain sediment transport at times of high rainfall; their association with palaeosols and desiccation cracks indicates seasonally wet to dry cycles throughout the Tournaisian. Tetrapod and fish fossils derived from floodplain lakes and land surfaces are concentrated by local erosion and reworking, and are preserved by deposition into temporary lakes on the floodplain; their distribution indicates a local origin, with sediment transported across the floodplain in seasonal rainfall episodes. These deposits are significant new sites that can be explored for the preservation of rare non-marine fossil material and provide unique insights into the evolution of early terrestrial ecosystems.

Funding

This study is a contribution to the TW:eed Project (Tetrapod World: early evolution and diversification), a major research programme investigating the rebuilding of Carboniferous ecosystems following a mass extinction at the end of the Devonian (Smithson et al., 2012). This study was funded by NERC Consortium Grant ‘The Mid-Palaeozoic biotic crisis: setting the trajectory of tetrapod evolution’ led by Professor Jenny Clack (University Museum of Zoology, Cambridge) and involving the Universities of Cambridge (NE/J022713/1), Leicester (NE/J020729/1), Southampton (NE/J021091/1), the British Geological Survey (NE/J021067/1) and the National Museum of Scotland.

History

Citation

Sedimentology, 2016, 63 (6), pp. 1677-1700 (24)

Author affiliation

/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Geology

Version

  • AM (Accepted Manuscript)

Published in

Sedimentology

Publisher

Wiley, International Association of Sedimentologists

issn

0037-0746

eissn

1365-3091

Acceptance date

2016-02-20

Copyright date

2016

Available date

2017-08-29

Publisher version

http://onlinelibrary.wiley.com/doi/10.1111/sed.12280/abstract

Language

en