TABLE 1. Summary counts of teleost centra from six vertebrate microfossil localities in the Tullock Member of the Fort Union Formation and one from the Ravenscrag Formation.
Mckeever Ranch 1 Loc V72210 |
% | Worm Coulee 1 Loc V74111 |
% | Morales 1 Loc V77128 |
% | Garbani 13 Loc V73080 |
% | Howards Biscuit Butte 2 Loc V81029 |
% | Yellow Sand Hill 8 Loc V75194 |
% | Pine Cree Loc. from RSM P1594 |
% | |
Coriops or Lopadichthys | 16 | 8.4 | 7 | 1.9 | 117 | 19 | 4 | 1 | 6 | 8 | 121 | 7 | ||
Gonorynchiform indet. type H | 60 | 3 | ||||||||||||
Notogoneus | 58 | 30.5 | 1 | 0.3 | 5 | 0.8 | 3 | 1 | 2 | 3 | 2 | 3 | 334 | 16 |
Teleost U3/BvD (K morph) | 1 | 0.3 | 2 | 0.3 | ||||||||||
Teleost U3/BvD (P morph) | 87 | 28 | 11 | 13 | 4 | 6 | 2 | 0.1 | ||||||
Estesesox | 1 | 0.5 | 2 | 0.5 | ||||||||||
Esox | 1 | 0.5 | 17 | 4.5 | 16 | 2.6 | 1 | 1 | 1 | 1 | 2 | 3 | 11 | 1 |
Acanthomorph centra type HC-1 | 2 | 0.3 | 1414 | 65 | ||||||||||
Acanthomorph centra type HC-2 | 108 | 56.8 | 312 | 83 | 259 | 42 | 211 | 67 | 59 | 74 | 52 | 85 | 166 | 8 |
Acanthomorph centra type HC-4 | 3 | |||||||||||||
Acanthomorph centra type AvE | 16 | 4.2 | 92 | 14.9 | 39 | 2 | ||||||||
Acanthomorph centra type HC-5 | 6 | 1.6 | 77 | 12.5 | ||||||||||
Teleost indet. type U-4 | 1 | 0.5 | 2 | 0.6 | 7 | 1.1 | 2 | 1 | ||||||
Teleost indet. type PT-1 | 5 | 2.6 | 8 | 2.1 | 38 | 6.2 | 2 | 1 | 1 | 1 | 2 | |||
Diplomystus | 4 | 0.2 | ||||||||||||
Total | 190 | 375 | 615 | 313 | 79 | 61 | 2151 |
Note: Centrum counts are calculated for each taxon/morphotype per locality and formation, with the grand total of all specimens listed in the lower right-hand corner. ∑Tu/taxon, total count per taxon from the Tullock Member; ∑total/taxon, total counts per taxon across Tullock Member and Ravenscrag Formation; comb., combination of specimens from all localities across the Tullock Member or both geologic units; Fm., formation; Mbr., member; Pu1, Pu2, and Pu3, Puercan 1, 2, and 3 North American Land Mammal “age” substages, respectively. The alternating white and grey rows represent the higher-level taxonomic groupings and sample sizes used in calculating the relative abundance patterns shown in the Paleogene portion of Figure 22.
TABLE 2. Stratigraphic distribution of teleost operational taxonomic units recognized here through the late Maastrichtian and Paleocene. Taxa known to be present in each time interval are shown in bold type. Taxa that can be inferred to be present during a time interval based on their presence in younger and older localities are shown in lower case.
Higher level taxon | Taxon/morphotype | late Maastricthian |
Pu1 | Pu2 | Pu3 | Ti | |
Elopomorpha | Elopiformes indet. | 1 | |||||
Elopomorpha | Phyllodus | 1 | 1 | 1 | 1 | ||
Osteoglossimorpha | Hiodontid (large-bodied taxon) | 1 | |||||
Osteoglossimorpha | Wilsonichthys ardinsulensis | 1 | |||||
Osteoglossimorpha | ? Wilsonichthys | 1 | |||||
Osteoglossimorpha | Ostariostoma | 1 | 1 | 1 | |||
Osteoglossimorpha | Coriops | 1 | 1 | 1 | 1 | ||
Osteoglossimorpha | aff. Lopadichthys/Lopadichthys | 1 | 1 | 1 | 1 | 1 | |
Osteoglossimorpha | Hiodontid sp. indet. | 1 | 1 | 1 | 1 | 1 | |
Osteoglossimorpha | Joffrichthys spp. | 1 | |||||
Clupeomorpha | Diplomystus | 1 | 1 | 1 | 1 | 1 | |
Ostariophyi | Otophysi indet. type U3/BvD (K morph) | 1 | 1 | ||||
Ostariophyi | Gonorynchiformes indet. type H | 1 | 1 | 1 | |||
Ostariophyi | Otophysi indet. type U3/BvD (P morph) | 1 | 1 | ||||
Ostariophyi | Notogoneus sp. | 1 | 1 | 1 | 1 | 1 | |
Ostariophyi | cypriniform indet. | 1 | |||||
Ostariophyi | Siluriformes | 1 | |||||
Protacanthopterygia | Estesesox | 1 | 1 | ||||
Protacanthopterygia | Esox sp. | 1 | 1 | 1 | 1 | ||
Protacanthopterygia | protacanthopterygian indet type ES1 | 1 | |||||
Protacanthopterygia | Speirsaenigma lindoei (Osmeridae) | 1 | |||||
Acanthomorpha | Acanthomorph HC-3 | 1 | |||||
Acanthomorpha | Acanthomorph HC-5 | 1 | 1 | ||||
Acanthomorpha | Acanthomorph type AvE | 1 | 1 | 1 | |||
Acanthomorpha | Lindoeichthys /aff. Lindoeichthys | 1 | 1 | 1 | 1 | ||
Acanthomorpha | Acanthomorph type HC-4 | 1 | 1 | 1 | 1 | ||
Acanthomorpha | Acanthomorph type HC-2 | 1 | 1 | 1 | 1 | ||
Acanthomorpha | aff. McConichthys | 1 | 1 | ||||
Acanthomorpha | “Priscacara” | 1 | 1 | 1 | 1 | ||
Acanthomorpha | Acanthomorph type HC-1 | 1 | 1 | 1 | 1 | 1 | |
Acanthomorpha | Acanthomorph type HC-6 | 1 | 1 | 1 | 1 | 1 | |
Acanthomorpha | Asineops | 1 | |||||
Acanthomorpha | Massamorichthys wilsoni | 1 | |||||
Acanthomorpha | Lateopisciculus turrifumosus | 1 | |||||
Teleost indet. | Teleost indet. type RvB | 1 | |||||
Teleost indet. | Teleost indet. type U-4 | 1 | 1 | 1 | 1 | ||
Teleost indet. | Teleost indet. type PT-1 | 1 | 1 | 1 | 1 | ||
Raw occurrence | 23 | 10 | 13 | 11 | 12 | ||
Range thru occurrence | 25 | 22 | 20 | 17 | 16 | ||
Minimum richness | 22 | 18 | 17 | 14 | 16 |
TABLE 3. Summary statistics of 14 teleost assemblages from the Lancian Hell Creek Formation and Puercan portions of the Fort Union (Tullock Member) and Ravenscrag formations.
Locality number | Locality name | NALMA | S | N | E | U95% | L95% |
UCMP V99220 | Tuma | L | 10 | 148 | 9.6 | 10.73 | 8.52 |
UCMP V99227 | Manzoni | L | 11 | 206 | 10.5 | 11.79 | 9.16 |
UCMP V99369 | Celeste's Magnificent Microsite | L | 14 | 188 | 12.4 | 14.5 | 10.31 |
UWBM C1153 | Hartless | L | 11 | 283 | 10.3 | 11.67 | 8.96 |
UWBM C1529 | Hot Feet | L | 8 | 126 | 8 | 8.23 | 7.74 |
UCMP V77130 | Hauso 1* | L | 10 | 51 | − | − | − |
UCMP V73087 | Flat Creek 5 | L | 14 | 700 | 11.4 | 13.4 | 9.41 |
UCMP V74111 | Worm Coulee 1 | Pu1 | 10 | 375 | 8 | 10.04 | 6.06 |
UCMP V77128 | Morales 1 | Pu1 | 10 | 615 | 8.2 | 9.99 | 6.36 |
UCMP V72210 | McKeever Ranch 1 | Pu1 | 7 | 190 | 6 | 7.57 | 4.34 |
RSM P1594 | Pine Cree Park | Pu2 | 9 | 2151 | 6.7 | 8.23 | 5.13 |
UCMP V75194 | Yellow Sand Hill 8* | Pu3 | 5 | 61 | − | − | − |
UCMP V81029 | Howard's Biscuit Butte 2* | Pu3 | 5 | 79 | − | − | − |
UCMP V73080 | Garbani 13-NW Harley's High | Pu3 | 8 | 313 | 6.1 | 8.18 | 4.01 |
Note: NALMA, North American Land Mammal “age”; S, raw number of operational taxonomic units (OTU); N, number of centra; E, estimated number of OTUs from rarefaction analysis of 124-specimen subsamples; U95%, estimated number of OTUs based on the upper 95% confidence interval via rarefaction analysis; L95%, estimated number of OTUs based on the lower 95% confidence interval via rarefaction analysis; UCMP, University of California Museum of Paleontology, Berekely, California, USA; RSM, Royal Saskatchewan Museum, Regina, Saskatchewan, Canada; UWBM, University of Washington Burke Museum of Natural History and Culture, Seattle, Washington, USA; L, Lancian NALMA; Pu1, Pu2, and Pu3, Puercan 1, 2, and 3 NALMA substages, respectively. Localities marked with an asterisk (*) were not analysed via rarefaction analysis due to their low sample sizes.