Where: Idaho (46.5° N, 116.8° W: paleocoordinates 46.4° N, 111.8° W)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Latah Formation, Langhian (16.0 - 13.8 Ma)
• Latah Formation overlies the Grande Ronde basalts (16-15.5 Ma; Barry et al., 2013), although younger parts of the Grande Ronde are absent at some localiies (Nash & Perkins, 2012). It underlies the Saddle Mountain basalts (c. 15 Ma and younger; Barry et al., 2013). Ash beds within the Latah Formation at White Bird, Idaho, are dated to 15.77 Ma (Mascall Tuff), 15.66 Ma (Bully Creek tuff), and an interpolated age of 14.3 Ma (Nash & Perkins, 2012).
• group of beds-level stratigraphic resolution
Environment/lithology: lacustrine - small; lithified mudstone
Size class: macrofossils
Preservation: mold/impression
Collected by S.E. Lewis in 1966; reposited in the UCM
• At least the Megachiline bee is deposited in University of Colorado Museum.
Primary reference: S. E. Lewis. 1969. Fossil insects of the Latah Formation (Miocene) of eastern Washington and northern Idaho. Northwest Science 43:99-115 [M. Clapham/M. Clapham/R. Day]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 97616: authorized by Matthew Clapham, entered by Matthew Clapham on 13.08.2010, edited by Jered Karr
Creative Commons license: CC BY (attribution)
Taxonomic list
Insecta | |
"Anisopus carolae n. sp." = Sylvicola carolae
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Bibio latahensis n. sp., Bibio testeus n. sp.
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Bolitophila pulveris n. sp.
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Sciara sepulta n. sp.
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Mycetophilidae indet., Mycetophilinae indet., Exechia juliaetta n. sp., "Rhymosia miocenica n. sp." = Rymosia miocenica, Boletina sp.2
Mycetophilidae indet. Newman 1834 fungus gnat
Mycetophilinae indet. Newman 1834 fungus gnat | |
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Pimplinae indet. Wesmael 1845 ichneumon wasp
Cryptinae indet. Kirby 1837 ichneumon wasp | |
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Macrophya adventitia n. sp.
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"Oreokora froeschneri n. sp." = Propentacora froeschneri
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Megaleuctra jewetti n. sp.
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