Buen Formation

The Buen Formation is a geologic formation and Lagerstätte in Peary Land, North Greenland. The shale preserves fossils dating back to the Early Cambrian period (Atdabanian in the local timescale, about 520 to 513 Ma).

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Buen Formation
Stratigraphic range: Cambrian Series 2 (Atdabanian)~
Formation
Sirius Passet
Upper & lower members
Hans Tavsen icecap
Portfjeld Formation
Up to 700 m (2,300 ft)
Mudstone
Sandstone, shale
.mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct,.mw-parser-output .geo-inline-hidden{display:none}.mw-parser-output .longitude,.mw-parser-output .latitude{white-space:nowrap}83°06′N 33°48′W / 83.1°N 33.8°W / 83.1; -33.8
22°06′S 49°00′W / 22.1°S 49.0°W / -22.1; -49.0
Peary Land
Greenland
Franklinian Basin
Southern Peary Land
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The Buen Formation is a geologic formation and Lagerstätte in Peary Land, North Greenland. The shale preserves fossils dating back to the Early Cambrian period (Atdabanian in the local timescale, about 520 to 513 Ma).

Geologic map of Sirius Passet with the Buen Formation shown in black

The oldest Cambrian series of the area was deposited in the Franklinian Basin and is poorly exposed in fragmentary, heavily metamorphosed outcrops in Peary Land. It was emplaced during the Ellesmerian orogeny.

Cambrian paleogeography with the Buen Formation in orange

During the Cambrian, Greenland was located in the southern tropical to temperate region. The Buen Formation forms part of the southern shelf succession of the Franklinian Basin of North Greenland and the Canadian Arctic Islands. The formation, approximately 325 metres (1,066 ft) thick, consists of a lower, sand−dominated, member overlain by an upper member dominated by dark grey−green mudstones and siltstones in its type area in southern Peary Land. It thickens to around 700 metres (2,300 ft) in northern Peary Land where it comprises a mud−rich transitional succession into deep water trough deposits of the Polkorridoren Group. Dark grey to black mudstones form part of this transitional succession from the shelf to the slope. To the south they lie in faulted contact with pale dolomites of the underlying Portfjeld Formation, and to the north with bioturbated mudstones and sandstones of the Buen Formation.

The following fossils have been reported from the formation:

GroupTaxonImageNotes
AnnelidsPhragmochaeta canicularis
ArthropodsBuenaspis forteyi
Buenellus
Aaveqaspis
Kerygmachela
Tamisiocaris
Limniphacos
Waptia
Kleptothule rasmusseni
Isoxys volucris
Hadranax augustus
Pauloterminus spinodorsalis
MolluscsHalkieria evangelista
DemospongesChoia hindei
OthersHeliosphaeridium dissimilare
Trapezovitus malinkyi
Kalaallitia myliuserichseni
Nasaaraqia hyptiotheciformis
Nevadotheca boerglumensis
Sullulika broenlundi
Alutella siku

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  • List of fossiliferous stratigraphic units in Greenland
  • Sirius Passet

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  • .mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"""""""'""'"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free.id-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited.id-lock-limited a,.mw-parser-output .id-lock-registration.id-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription.id-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#bf3c2c)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#bf3c2c)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}Peel, John S.; Willman, Sebastian (2018), "The Buen Formation (Cambrian Series 2) biota of North Greenland", Papers in Palaeontology, 4 (3): 381–432, Bibcode:2018PPal....4..381P, doi:10.1002/spp2.1112

  • Geyer, Gerd; Peel, John S. (2011), "The Henson Gletscher Formation, North Greenland, and its bearing on the global Cambrian Series 2-Series 3 boundary" (PDF), Bulletin of Geosciences, 86: 465–534, doi:10.3140/bull.geosci.1252

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  • Higgins, A.K.; Soper, N.J.; Leslie, A.G. (2000), "The Ellesmerian and Caledonian Orogenie Belts of Greenland" (PDF), Polarforschung, 68: 141–151

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  • G. E. Budd and J. S. Peel. 1998. A new xenusiid lobopod from the Early Cambrian Sirius Passet fauna of North Greenland. Palaeontology 41(6):1201-1213

  • J. K. Rigby. 1986. Cambrian and Silurian sponges from North Greenland. Rapport Groenlands Geologiske Undersoegelse 132:51-63

  • M. Williams, D. J. Siveter, and J. S. Peel. 1996. Isoxys (arthropoda) from the Early Cambrian Sirius Passet Lagerstaette, North Greenland. Journal of Paleontology 70(6):947-954

  • S. Conway Morris and J. S. Peel. 1990. Articulated halkieriids from the Lower Cambrian of north Greenland. Nature 345(28):802-805