{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,30]],"date-time":"2026-04-30T14:32:46Z","timestamp":1777559566134,"version":"3.51.4"},"reference-count":101,"publisher":"Geological Society of London","issue":"6","license":[{"start":{"date-parts":[[2020,8,11]],"date-time":"2020-08-11T00:00:00Z","timestamp":1597104000000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2020,11]]},"abstract":"<jats:p>The Mesozoic\u2013Cenozoic separation of Greenland and North America produced the small oceanic basins of the Labrador Sea and Baffin Bay, connected via a complex transform system through the Davis Strait. During rifting and partial breakup sedimentary basins formed that record the changing regional sediment supply. The onshore and offshore stratigraphy of Central West Greenland outlines the presence of a major fluvial system that existed during the Cretaceous and was later redirected in the Early Cenozoic by the formation of the West Greenland Igneous Province. Hydrological analysis of Greenland's isostatically balanced basement topography outlines two major drainage systems that likely flowed across Greenland prior to the onset of glaciation and emptied into the Sisimiut Basin within the Davis Strait, offshore West Greenland. The course of the northern drainage system suggests that it initially flowed NW into the Cretaceous\/Palaeocene Nuussuaq Basin, before being redirected SW around the West Greenland Igneous Province in the Mid-Palaeocene. Moreover, characteristics of these two drainage systems suggest they acted as a single larger fluvial system, prior to the onset of glaciation, that was likely the primary source of sediment across Central West Greenland throughout the Cretaceous and Palaeogene. This scenario provides a greater understanding of the West Greenland margin's late Cenozoic evolution, which differs from previous interpretations that hypothesize a period of considerable post-rift tectonism and uplift. This work highlights the importance of large pre-glacial drainage systems across North Atlantic passive margins and their relevance when studying post-rift stratigraphy in rifted margin settings.<\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            Isostatic modelling, hydrological analysis and chi mapping is available at:\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.5050146\">https:\/\/doi.org\/10.6084\/m9.figshare.c.5050146<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2020-028","type":"journal-article","created":{"date-parts":[[2020,7,8]],"date-time":"2020-07-08T15:27:27Z","timestamp":1594222047000},"page":"1149-1160","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":5,"title":["Sediment supply on the West Greenland passive margin: redirection of a large pre-glacial drainage system"],"prefix":"10.1144","volume":"177","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-1960-2901","authenticated-orcid":false,"given":"Scott","family":"Jess","sequence":"first","affiliation":[{"name":"Department of Geoscience, University of Calgary, Calgary, Alberta Canada T2N 1N4"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7846-3898","authenticated-orcid":false,"given":"Alexander L.","family":"Peace","sequence":"additional","affiliation":[{"name":"McMaster University, School of Earth Environment and Society, Hamilton, ON, Canada"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Christian","family":"Schiffer","sequence":"additional","affiliation":[{"name":"Department of Earth Sciences, Uppsala University, 752 36 Uppsala, Sweden"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1881","published-online":{"date-parts":[[2020,8,11]]},"reference":[{"key":"e_1_3_5_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.tecto.2018.08.002"},{"key":"e_1_3_5_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.quascirev.2010.02.007"},{"key":"e_1_3_5_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.tecto.2009.04.006"},{"key":"e_1_3_5_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.marpetgeo.2018.06.030"},{"key":"e_1_3_5_6_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.1239794"},{"key":"e_1_3_5_7_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.1249047"},{"key":"e_1_3_5_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.marpetgeo.2017.04.015"},{"key":"e_1_3_5_9_1","volume-title":"Principles of sequence stratigraphy","author":"Catuneanu O.","year":"2006","unstructured":"Catuneanu, O. 2006. 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