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- Q5477838 subject Q8375757.
- Q5477838 abstract "The Fram Formation is a Late Devonian sequence of rock strata on Ellesmere Island that came into prominence in 2006 with the discovery in its rocks of examples of the transitional fossil, Tiktaalik, a sarcopterygian or lobe-finned fish showing many tetrapod characteristics. The Fram Formation is a Middle to Upper (Late) Devonian clastic wedge forming an extensive continental facies consisting of sediments derived from deposits laid down in braided stream systems that formed some 375 million years ago, at a time when the North American craton ("Laurentia") was straddling the equator.".
- Q5477838 wikiPageExternalLink Daeschler_tetrapod_nat06.pdf.
- Q5477838 wikiPageWikiLink Q131481.
- Q5477838 wikiPageWikiLink Q146841.
- Q5477838 wikiPageWikiLink Q160830.
- Q5477838 wikiPageWikiLink Q191110.
- Q5477838 wikiPageWikiLink Q19159.
- Q5477838 wikiPageWikiLink Q447188.
- Q5477838 wikiPageWikiLink Q49.
- Q5477838 wikiPageWikiLink Q590219.
- Q5477838 wikiPageWikiLink Q65955.
- Q5477838 wikiPageWikiLink Q8375757.
- Q5477838 wikiPageWikiLink Q858071.
- Q5477838 comment "The Fram Formation is a Late Devonian sequence of rock strata on Ellesmere Island that came into prominence in 2006 with the discovery in its rocks of examples of the transitional fossil, Tiktaalik, a sarcopterygian or lobe-finned fish showing many tetrapod characteristics.".
- Q5477838 label "Fram Formation".