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Depositional system and plant ecosystem responses to long-term low tempo volcanism, the Interbasaltic Formation, Antrim Lava Group

Beresford-Browne, Adam; Jolley, David; Millett, John; Stevenson, Carl; Watt, Sebastian; Raine, Rob; Carter, Elliot

Authors

Adam Beresford-Browne

David Jolley

John Millett

Carl Stevenson

Sebastian Watt

Rob Raine



Abstract

The Antrim Lava Group of NE Ireland comprises a volcanic sequence dominated by basaltic lava flows. Including subsidiary sedimentary interlayers and some evolved lavas and intrusions, the overall sequence reaches a cumulative thickness of ∼800 m. The tempo of eruption of the Antrim Lava Group is poorly constrained but can be evaluated via weathering patterns and environmental reconstructions derived from lava-flow interbeds. In this contribution, we present palynology from a newly identified and well-developed 2.0–2.5 m thick sedimentary sequence (interbed) at Ross's Quarry, Ballycastle, Co. Antrim, that helps elucidate the contemporary development of environments in a setting subject to periodic basaltic volcanism. The interbed is subdivided into geologically distinct subunits of cross-bedded and parallel-bedded sandstones and sandy siltstones, all rich in visible organic remains such as rootlets and fragments of wood and bark. A total of 19 samples was collected from the sequence and subsequently analysed for palynological content. The palynomorph data point toward a diversity of inputs ranging from estuaries, chalky soils, dry soils, swamps, lakes, floodplains, sand bars, wet soils, established bogs and fenlands. In contrast to current understanding, the palynological data and their inferred environments collectively reveal the presence of flora that favour a temperate climate rather than the subtropical climate that has previously been inferred from the lateritic interbeds of the Antrim Lava Group. By combining the Ross's Quarry observations with palynological data from other quarry sites and boreholes in Antrim, we provide new insights into the climate, weathering systems and eruptive history of the Antrim Lava Group.

Citation

Beresford-Browne, A., Jolley, D., Millett, J., Stevenson, C., Watt, S., Raine, R., & Carter, E. (2024). Depositional system and plant ecosystem responses to long-term low tempo volcanism, the Interbasaltic Formation, Antrim Lava Group. Geological Society Special Publications, 547(1), 483-509. https://doi.org/10.1144/sp547-2023-75

Journal Article Type Article
Acceptance Date Aug 8, 2024
Online Publication Date Mar 8, 2024
Publication Date Aug 9, 2024
Deposit Date Nov 13, 2024
Journal Geological Society, London, Special Publications
Print ISSN 0305-8719
Electronic ISSN 2041-4927
Publisher The Geological Society
Peer Reviewed Peer Reviewed
Volume 547
Issue 1
Pages 483-509
DOI https://doi.org/10.1144/sp547-2023-75
Public URL https://keele-repository.worktribe.com/output/976086
Publisher URL https://www.lyellcollection.org/doi/full/10.1144/SP547-2023-75
Additional Information Received: 2023-04-28; Revised: 2023-11-07; Accepted: 2023-11-07; Published: 2024-03-08