The Palaeoproterozoic global carbon cycle: insights from the Loch Maree Group, NW Scotland

Gemma B. Kerr, Anthony R. Prave, Adam P. Martin, Anthony E. Fallick, Alexander T. Brasier, R. Graham Park

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6 Citations (Scopus)
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Two Palaeoproterozoic events have particularly interested Earth scientists. These are the global Lomagundi–Jatuli Event, the greatest magnitude positive carbonate carbon isotope excursion in Earth history, and the Shunga Event, the world’s largest organic carbon burial event. Analysis of newly acquired high-resolution C–O isotope data and U–Pb zircon geochronology refine understanding of carbon isotope characteristics and timing of deposition of the Palaeoproterozoic Loch Maree Group of NW Scotland. Petrographic examination reveals a basal unconformity between the Loch Maree Group and Archaean basement, permitting a stratigraphy and younging direction to be assigned. Detrital zircon ages from immediately above the unconformity are dated at c. 2.3 Ga. δ13Ccarbonate data on two temporally discrete carbonate packages range from c. +15 to 2‰ in the older unit and c. 2 to −5‰ in the younger carbonate unit. Current age constraints indicate that the Loch Maree Group is too young to be fully coeval with the Lomagundi–Jatuli Event but is within the age range of the Shunga Event. This revives consideration of a straightforward mass-balance process involving burial of organic carbon as an explanation for at least some of the C-cycle perturbations of Palaeoproterozoic time.
Original languageEnglish
Pages (from-to)170-176
Number of pages7
JournalJournal of the Geological Society
Issue number1
Early online date22 Sept 2015
Publication statusPublished - Jan 2016

Bibliographical note

Fieldwork was supported by the Edinburgh Geological Society Clough &
Mykura Fund, the Carnegie Undergraduate Scholarship and a stipend provided
by the Irvine Bequest through the University of St Andrews to G.B.K.
Laboratory work, and isotope and geochronology analyses were financed by
NERC grant NE/G00398X/1 to A.R.P., A.E.F., D.J.Condon and A.P.M. Thanks
go to T. Donnelly, J. Dougans, A. Calder, D. Herd, B. Pooley and A. Mackie for
laboratory assistance.


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