Files in this item
A marine origin for the late Mesoproterozoic Copper Harbor and Nonesuch Formations of the Midcontinent Rift of Laurentia
Item metadata
dc.contributor.author | Jones, S.M. | |
dc.contributor.author | Prave, A.R. | |
dc.contributor.author | Raub, T.D. | |
dc.contributor.author | Cloutier, J. | |
dc.contributor.author | Stüeken, E. E. | |
dc.contributor.author | Rose, C.V. | |
dc.contributor.author | Linnekogel, S. | |
dc.contributor.author | Nazarov, K. | |
dc.date.accessioned | 2020-11-09T00:38:29Z | |
dc.date.available | 2020-11-09T00:38:29Z | |
dc.date.issued | 2020-01 | |
dc.identifier | 263520783 | |
dc.identifier | 6209cbe8-84af-4f06-a32b-3ffb9b0e5362 | |
dc.identifier | 85074660390 | |
dc.identifier | 000508748600014 | |
dc.identifier.citation | Jones , S M , Prave , A R , Raub , T D , Cloutier , J , Stüeken , E E , Rose , C V , Linnekogel , S & Nazarov , K 2020 , ' A marine origin for the late Mesoproterozoic Copper Harbor and Nonesuch Formations of the Midcontinent Rift of Laurentia ' , Precambrian Research , vol. 336 , 105510 . https://doi.org/10.1016/j.precamres.2019.105510 | en |
dc.identifier.issn | 0301-9268 | |
dc.identifier.other | RIS: urn:EEF07978995850D4FCB9E80E2A8A1B79 | |
dc.identifier.other | ORCID: /0000-0002-4614-3774/work/65013838 | |
dc.identifier.other | ORCID: /0000-0002-9432-9880/work/65014386 | |
dc.identifier.other | ORCID: /0000-0001-6861-2490/work/65014397 | |
dc.identifier.other | ORCID: /0000-0001-8149-0977/work/65014453 | |
dc.identifier.other | ORCID: /0000-0003-4513-2245/work/84315167 | |
dc.identifier.uri | https://hdl.handle.net/10023/20926 | |
dc.description | This work was supported by First Quantum Minerals Ltd., Vancouver, Canada. | en |
dc.description.abstract | The c. 1.1 Ga Copper Harbor and Nonesuch Formations of the Keweenawan Supergroup exposed along the Canadian-United States shorelines of Lake Superior are part of the surface exposures of the Laurentian Midcontinent Rift. These units have long been considered non-marine in origin and have figured prominently in ideas regarding the evolution of microbial life and the redox conditions of Earth’s ocean-atmosphere system at the close of Mesoproterozoic time. However, these rocks also host hydrothermal metal deposits, the emplacement of which may have compromised primary geochemical signals that are used to underpin those ideas. Here we highlight new sedimentological observations to provide an independent framework for assessing the depositional setting and geochemistry of those strata. We show that the totality of sedimentological features leads to the conclusion that parts of the upper Copper Harbor Formation and the entirety of the Nonesuch Formation were deposited along tide- and wave-influenced shorelines and in shallow-marine settings under evaporitic conditions. Evidence for this interpretation includes the abundance of flaser, wavy, linsen and pinstripe bedding, ubiquity of reactivation surfaces and mud drapes associated with all ripple forms, superposed sets of ripple cross-lamination showing bimodal (herring-bone) sediment transport directions, desiccation cracks and metre-scale hummocky cross-stratification. Further, evaporite fabrics and pseudomorphs after gypsum in the upper 200 m of the Copper Harbor Formation and in numerous stratigraphic positions within the Nonesuch Formation indicate that the water body was saline, not fresh. The emerging palaeogeographic image is one of a large, shallow-marine embayment with fringing sabkha-like shorelines. Ideas about late Mesoproterozoic biospheric evolution and Earth’s surface redox and oxygenation that rely on the Nonesuch Formation and Copper Harbor stromatolites having been deposited within a lacustrine setting require reassessment. | |
dc.format.extent | 7108993 | |
dc.language.iso | eng | |
dc.relation.ispartof | Precambrian Research | en |
dc.subject | Midcontinent Rift | en |
dc.subject | Keweenawan Supergroup | en |
dc.subject | Copper Harbor Formation | en |
dc.subject | Nonesuch Formation | en |
dc.subject | Lacustrine | en |
dc.subject | Mesoproterozoic | en |
dc.subject | GE Environmental Sciences | en |
dc.subject | DAS | en |
dc.subject | SDG 14 - Life Below Water | en |
dc.subject.lcc | GE | en |
dc.title | A marine origin for the late Mesoproterozoic Copper Harbor and Nonesuch Formations of the Midcontinent Rift of Laurentia | en |
dc.type | Journal article | en |
dc.contributor.institution | University of St Andrews. School of Earth & Environmental Sciences | en |
dc.contributor.institution | University of St Andrews. Scottish Oceans Institute | en |
dc.contributor.institution | University of St Andrews. St Andrews Sustainability Institute | en |
dc.contributor.institution | University of St Andrews. St Andrews Isotope Geochemistry | en |
dc.contributor.institution | University of St Andrews. Marine Alliance for Science & Technology Scotland | en |
dc.contributor.institution | University of St Andrews. St Andrews Centre for Exoplanet Science | en |
dc.identifier.doi | 10.1016/j.precamres.2019.105510 | |
dc.description.status | Peer reviewed | en |
dc.date.embargoedUntil | 2020-11-09 |
This item appears in the following Collection(s)
Items in the St Andrews Research Repository are protected by copyright, with all rights reserved, unless otherwise indicated.