Show simple item record

dc.contributor.authorWilson, Edward C.
dc.date.accessioned2020-09-03T11:29:30Z
dc.date.available2020-09-03T11:29:30Z
dc.identifier.urihttps://scholar.oxy.edu/handle/20.500.12711/10852
dc.description.abstractThe spiral trace fossil Gyrolithes de Saporta, 1884 in the Pliocene Tirabuzon Formation near Santa Rosalia, Baja California Sur, Mexico, by Edward C. Wilson. Bull. Southern California Acad. Sci., 84(2):57-66, 1985. The largest recorded specimens of the enigmatic spiral trace fossil Gyrolithes are abundant in the Pliocene Tirabuzon Formation near Santa Rosalia, Baja California Sur, Mexico. They grade gradually into Thalassinoides-type burrows. Both types of burrows are lined by scratch marks, suggesting excavation by a decapod crustacean. Associated mollusks indicate a depth of 55 to 90 m.
dc.subjectSpiral Trace Fossil
dc.subjectGyrolithes de Saporta
dc.subjectPliocene Tirabuzon Formation
dc.subjectSanta Rosalia
dc.subjectBaja California Sur
dc.subjectMexico
dc.titleThe Spiral Trace Fossil Gyrolithes de Saporta, 1884 in the Pliocene Tirabuzon Formation Near Santa Rosalia, Baja California Sur, Mexico
dc.title.alternativeGyrolithes De Saporta
dc.typearticle
dc.abstract.formatonep
dc.source.beginpage57
dc.source.issuescas/vol84/iss2
dc.source.issue2
dc.identifier.legacyhttps://scholar.oxy.edu/scas/vol84/iss2/7
dc.source.endpage66
dc.source.peer_reviewedTRUE
dc.source.statuspublished
dc.source.volume84
dc.source.journaltitleScas: Bulletin of the Southern California Academy of Sciences


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record