Palynological data from Loch an t’Suidhe, Isle of Mull, Scotland

Introduction Pollen and non-pollen palynomorph data from the Isle of Mull, Inner Hebrides, Scotland are presented from the site of Loch an t’Suidhe, a small lake on the Ross of Mull peninsula. The aim was to determine the palaeoecological record associated with early to mid-Holocene environmental change. Methods A core was extracted from the infilled peaty margins at the southern end of the loch with an 8 cm diameter Russian-type corer. Pollen, spore, non-pollen palynomorph, microscopic charcoal and loss-on-ignition data derive from the basal part of the core. Six radiocarbon dates contribute to core chronology. Dates are calibrated using the IntCal20 calibration curve with age-depth modelling via Clam software. Palynomorph data are produced using Tilia and TGView software. Results The profile covers the Holocene period from an estimated 10890–5470 calendar years BP. Discussion The data enable comparisons to be made with undated palynological profiles already available from the Isle of Mull, enhancing opportunities to explain early to mid-Holocene environmental change – which would cover the Mesolithic and early Neolithic archaeological periods – in the Inner Hebrides and beyond.

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Journal
Palynology
Published
2026-04-21
DOI
https://doi.org/10.1080/01916122.2026.2658690
Primary Topic
Geology and Paleoclimatology Research
Type
article
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article

Palynological data from Loch an t’Suidhe, Isle of Mull, Scotland

Heather Sugden, J. Edward Schofield, James B. Innés, Kevin J. Edwards et al.
Palynology
Geology and Paleoclimatology Research
article

Palynological data from Loch an t’Suidhe, Isle of Mull, Scotland

Heather Sugden, J. Edward Schofield, James B. Innés, Kevin J. Edwards, Jeff Blackford
article en

Abstract

Introduction Pollen and non-pollen palynomorph data from the Isle of Mull, Inner Hebrides, Scotland are presented from the site of Loch an t’Suidhe, a small lake on the Ross of Mull peninsula. The aim was to determine the palaeoecological record associated with early to mid-Holocene environmental change. Methods A core was extracted from the infilled peaty margins at the southern end of the loch with an 8 cm diameter Russian-type corer. Pollen, spore, non-pollen palynomorph, microscopic charcoal and loss-on-ignition data derive from the basal part of the core. Six radiocarbon dates contribute to core chronology. Dates are calibrated using the IntCal20 calibration curve with age-depth modelling via Clam software. Palynomorph data are produced using Tilia and TGView software. Results The profile covers the Holocene period from an estimated 10890–5470 calendar years BP. Discussion The data enable comparisons to be made with undated palynological profiles already available from the Isle of Mull, enhancing opportunities to explain early to mid-Holocene environmental change – which would cover the Mesolithic and early Neolithic archaeological periods – in the Inner Hebrides and beyond.

Palynology
University of Dundee (GB), Durham University (GB), Arthur B. McDonald-Canadian Astroparticle Physics Research Institute (CA), Institute of Geography (KZ), Department of Archaeology (LK), University of Sheffield (GB)
Openalex Percentile: Top 14%
Geology and Paleoclimatology Research
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