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Specimen Record

ContinentNorth America
CountryUnited States
State/ProvinceOklahoma
County/ParishMurray(?)
LocalityWhite Mound, S Of Sulphur
Latitude34.37222
Longitude-97.0075
Institution CodeKu
Collection CodeKumip
Catalog Number136938

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 Julien Kimmig
RoleCollection Manager
Emailjkimmig@ku.edu
Name Julien Kimmig
RoleCollection Manager
Emailjkimmig@ku.edu
Name Laura Russell
RoleVertNet Programmer
Emaillarussell@ku.edu
Name Bruce Lieberman
RoleCurator
Emailblieber@ku.edu
  • Data
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Taxonomy
Scientific NameMeristella atoka
KingdomAnimalia
PhylumBrachiopoda
ClassRhynchonellata
OrderAthyridida
FamilyMeristellidae
GenusMeristella
Specific Epithetatoka
Specimen
Catalog Number136938
Institution CodeKU
Collection CodeKUMIP
Occurrence ID2623c4e0-1ed8-11e3-bfac-90b11c41863e
Dataset NameUniversity of Kansas Biodiversity Institute invertebrate paleontology collection
Basis of RecordFossilSpecimen
Type of ResourcePhysicalObject
Locality
CountryUnited States
State / ProvinceOklahoma
CountyMurray(?)
Higher GeographyUnited States, Oklahoma, Murray(?)
ContinentNorth America
LocalityWhite Mound, S of Sulphur
Decimal Latitude34.3722200
Decimal Longitude-97.0075000
Coordinate Uncertainty In Meters570.0000000000
Geodetic DatumWGS84
Georeference RemarksWhite Mound is located almost exactly in the center of the NE quadrant of Section 20. We plotted White Mound in Google Earth and drew a line to the furthest corner of the NE quadrant. This ended up equating to the standard TRS error.
Georeferenced ByFarrell, Una C
Georeferenced Date2012-08-21
Paleo Context
Geological Context GroupHunton Group
FormationHaragan Shale
Earliest Period Or Lowest SystemDevonian
Earliest Epoch Or Lowest SeriesLower Devonian
Other
Languageen
Modified2014-09-22 10:25:27.0
ID2623c4e0-1ed8-11e3-bfac-90b11c41863e
dwc:datasetID0938172b-2086-439c-a1dd-c21cb0109ed5
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