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Specimen Record

ContinentNorth America
CountryUnited States
State/ProvinceTexas
County/ParishPalo Pinto
LocalityCut On Us 80, 4.1 Miles West Of Center Of Mineral Wells
Latitude32.798282
Longitude-98.184205
Institution CodeKu
Collection CodeKumip
Catalog Number359740

From Recordset

http://biodiversity.ku.edu/invertebrate-paleontology/collections

The University of Kansas invertebrate paleontology collection is ranked among the top 10 largest fossil invertebrate collections in the country and has over 850,000 fossil invertebrate and microfossil specimens from all over the world, including more than 8,200 type or figured specimens. These specimens have been used for research by paleontologists for over 120 years. The collection has taxonomic strengths in Cambrian trilobites from Antarctica and the Great Basin, United States; Upper Paleozoic invertebrates of the mid-continent; Cambrian soft-bodied faunas from Utah; Mesozoic cephalopods from the mid-continent. Research access to the collections is arranged on a case-by-case basis.

Contacts

Name Una Farrell
RoleCollection Manager
Emailufarrell@ku.edu
Name Una Farrell
RoleCollection Manager
Emailufarrell@ku.edu
Name Laura Russell
RoleVertNet Programmer
Emaillarussell@ku.edu
Name Bruce Lieberman
RoleCurator
Emailblieber@ku.edu
  • Data
  • Flags
  • Raw
Taxonomy
Scientific NameCrinoidea
KingdomAnimalia
PhylumEchinodermata
ClassCrinoidea
Genuscarinoidea
Specimen
Catalog Number359740
Institution CodeKU
Collection CodeKUMIP
Occurrence ID08b49025-cbfe-4c4c-a4e0-e524a69f6ce2
Dataset NameUniversity of Kansas Biodiversity Institute invertebrate paleontology collection
Basis of RecordFossilSpecimen
Type of ResourcePhysicalObject
Locality
CountryUnited States
State / ProvinceTexas
CountyPalo Pinto
Higher GeographyUnited States, Texas, Palo Pinto
ContinentNorth America
LocalityCut on US 80, 4.1 miles west of center of Mineral Wells
Decimal Latitude32.798282
Decimal Longitude-98.184205
Coordinate Uncertainty In Meters12852.0000000000
Geodetic DatumWGS84
Georeference RemarksGeoLocate used to determine 4.1 miles from center of Mineral Wells. The point was then moved to be on HWY 180 (formerly US 80), which corresponds to a visible outcrop on Google Earth. Uncertainty from GeoLocate.
Georeferenced BySaupe, Erin
Georeferenced Date2012-09-14
Paleo Context
Geological Context GroupStrawn
MemberKeechi Creek?
FormationMineral Wells Formation
Earliest Period Or Lowest SystemPennsylvanian
Earliest Epoch Or Lowest SeriesMiddle Pennsylvanian
Earliest Age Or Lowest StageDesmoinesian
Other
Languageen
Modified2014-09-22 10:26:14.0
ID08b49025-cbfe-4c4c-a4e0-e524a69f6ce2
dcterms:accessRightshttp://biodiversity.ku.edu/research/university-kansas-biodiversity-institute-data-publication-and-use-norms
dcterms:licensehttp://creativecommons.org/licenses/by/4.0/deed.en_US
dwc:institutionIDhttp://grbio.org/cool/iakn-125z
specimen list