Allenby Formation | |
---|---|
Stratigraphic range: Ypresian | |
Type | Geological formation |
Unit of | Princeton Group, Eocene Okanagan Highlands |
Sub-units | Princeton Chert, Vermillion Bluffs Shale |
Overlies | Cedar Formation |
Area | 300 km2 (120 sq mi) [1] |
Thickness | 1,860–2,100 m (6,100–6,890 ft) [1] |
Lithology | |
Primary | Shale, sandstone |
Other | Coal–breccia, coal–chert |
Location | |
Coordinates | 49°22.6′N120°32.8′W / 49.3767°N 120.5467°W |
Approximate paleocoordinates | 53°06′N107°30′W / 53.1°N 107.5°W |
Region | British Columbia |
Country | Canada |
Extent | Princeton Basin & Tulameen basin |
Type section | |
Named for | Allenby, British Columbia |
Named by | Shaw |
Year defined | 1952 |
The Allenby formation is a sedimentary rock formation in British Columbia which was deposited during the Ypresian stage of the Early Eocene. It consists of conglomerates, sandstones with interbedded shales and coal. The shales contain an abundance of insect, fish and plant fossils known from 1877 and onward, while the Princeton Chert was first indented in the 1950s and is known from anatomically preserved plants.
There are several notable fossil producing localities in the Princeton & Tulameen basins. Historical collection sites included Nine Mile Creek, Vermilian Bluffs, and Whipsaw Creek, while modern sites include One Mile Creek, Pleasant Valley, Thomas Ranch, and the Princeton Chert.
The Allenby is estimated to have an overall extent of approximately 300 km2 (120 sq mi), though actual outcroppings of the formation make up less than 1% of the formation, while other exploratory contact is via boreholes and mines. The half-graben which contains the formation is separated into two major depositional basins, the Princeton basin around Princeton, British Columbia and the Tulameen basin centered approximately 17 km (11 mi) west. The grabens extensional faults at the eastern side of the basin place the hanging wall Allenby strata in contact with much older foot wall strata of the Nicola Formation which dates to the Upper Triassic. [1] [2] [3]
The Allenby Formation is the southern-most of the Eocene Okanagan Highlands lakes in British Columbia, and second most southern site after the Klondike Mountain Formation of Republic, Washington and northern Ferry County. In British Columbia, the formation is coeval to the Tranquille Formation, known from the McAbee Fossil Beds and Falkland site, the Coldwater Beds, known from the Quilchena site, and Driftwood Canyon Provincial Park. The highlands, including the Allenby Formation, have been described as one of the "Great Canadian Lagerstätten " [4] based on the diversity, quality and unique nature of the biotas that are preserved. The highlands temperate biome preserved across a large transect of lakes recorded many of the earliest appearances of modern genera, while also documenting the last stands of ancient lines. [4]
The warm temperate uplands floras of the Allenby Formation and the highlands, associated with downfaulted lacustrine basins and active volcanism are noted to have no exact modern equivalents, due to the more seasonally equitable conditions of the Early Eocene. However, the formation has been compared to the upland ecological islands in the Virunga Mountains within the Albertine Rift of the African rift valley. [5]
The earliest work in the region was on exploratory expeditions in 1877 and 1878, with fossils collected in the areas of Nine-Mile Creek, Vermilian Bluffs on the Similkameen River, and Whipsaw Creek. While reporting on additional plant fossils collected from British Columbia, Penhallow (1906) noted the likely coeval status of the Princeton basins with many of the sites now considered the Okanagan Highlands. [6] Modern collecting has centered on the areas around One Mile Creek, Pleasant Valley, and Thomas Ranch. [2]
The age estimates for the Allenby Formation have varied a number of times since the first explorations happened in the 1870s. Shaw (1952) dated the formation as Oligocene, an age followed by Arnold (1955). [7] [8] Half a decade later, the older age of 48 ± 2 million years old was first suggested, with a younger age being suggested at 46.2 ± 1.9 million years old in 2000 and an older date of 52.08 ± 0.12 million years ago obtained from uranium–lead dating of zircons from Vermilion Bluffs shale in 2005. [1]
The Allenby is composed of cyclical sedimentation events that were deposited along the course of a river-system in conjunction with depositional areas from nearby lakes and wetlands. Coeval volcanic eruptive events are recorded as interbeds of tephras and lavas, while the riverine course is marked with depositional areas of conglomerates and sandstones. The quieter environments are noted for finer layers of shales and coalified layers. [1]
The coal seams throughout the formation are typically sub-bituminous. [1]
Notable in conjunction with the coal seams are sections of chert which formed during silica rich periods. The rapid cyclical changes from coal to chert and back are not noted in any other fossil locality in the world. An estimated 49 coal-chert cycles are known, though the exact conditions for this process are not well understood. Silica rich volcanic episodes in the region during deposition would have been needed for formation of the cherts, while slowly moving waters and gently subsiding terrains would be needed for the peats and fens to accumulate. Rates of organic deposition in swamps have been estimated at 0.5–1 mm (0.020–0.039 in) in modern temperate climates, this suggests the time needed for each 10–20 cm (3.9–7.9 in) chert layer would be at least 100 years or more, with the full sequence of cycles taking place over no more than 15,000 years. [1]
Palynological analysis of samples from the Thomas ranch site by Dillhoff et al. (2013) resulted in the identification of 32 pollen and spore types that were assignable to family or genus level, with a total number of distinct pollen and spore types, including unassignable morphotypes, number over 70. The predominant pollens of the site are conifers, which make up between 85%–97% of the total pollens, while the angiosperm pollens are dominated by members of Betulaceae. [2]
Several pteridophyte families and genera are represented as spore fossils alone, without corresponding megafossil records, including Lycopodiaceae, Osmundaceae, and Schizaeaceae. Similarly, at least three additional conifer genera are only present as pollen fossils and up to 12 angiosperms are present in the pollen record. Sometimes considered a Biostratgraphic index fossil, the angiosperm palynospecies Pistillipollenites macgregorii has been recovered from several sites in the Allenby Formation, while the palynospecies Erdtmanipollis pachysandroides is rare, having only been reported from the formation twice. [2]
Family | Genus | Species | Pollen/Macrofossil | Notes | Images |
---|---|---|---|---|---|
Unidentified [2] | Pollen | A holly palynomorph | |||
Pollen | A palm palynomorph | ||||
Pollen | A box family palynomorph | ||||
Unidentified [2] | Pollen & macrofossils | An alder palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A birch palynomorph | |||
Unidentified [2] | Pollen | A hornbeam palynomorph | |||
unidentified [2] | Pollen | A hazelnut palynomorph | |||
unidentified [2] | Pollen | A Cunninghamia like palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A redwood palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A Taxodioideae subfamily palynomorph | |||
Unidentified [2] | Pollen | An elaeagnaceous palynomorph, similar to oleaster | |||
unidentified | Unidentified [2] | Pollen | An ericaceous palynomorph of uncertain affinity | ||
Unidentified [2] | Pollen | A chestnut palynomorph | |||
Unidentified [9] | Pollen | A fagaceous palynomorph | |||
"Fagus Pollen type 3" [9] | Pollen | A beech palynomorph | |||
"Fagus Pollen type 2" [9] | Pollen | A beech palynomorph | |||
Pollen | A fagaceous palynomorph | ||||
"Quercus Pollen type 1" [9] | Pollen | An oak palynomorph, similar to Quercus Group Lobatae pollen | |||
"Quercus Pollen type 2" [9] | Pollen | An oak palynomorph, ancestral type with Quercus Group Ilex morphology | |||
Unidentified [9] | Pollen | A fagaceous palynomorph | |||
Unidentified | Unidentified [9] | Pollen | A Fagoideceous palynomorph | ||
Unidentified [2] | Pollen | ||||
Pollen & macrofossils | A Gingko palynomorph | ||||
Unidentified [2] | Pollen | A sweet gum palynomorph | |||
Unidentified [2] | Pollen | A hickory palynomorph | |||
Unidentified [2] | Pollen | A hickory palynomorph | |||
Unidentified [2] | Pollen | A lycopod palynomorph | |||
Unidentified [2] | Pollen | A linden palynomorph | |||
Unidentified [2] | Pollen | An osmundaceous fern palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A fir palynomorph | |||
Unidentified [2] | Pollen | A pine family palynomorph | |||
Unidentified [2] | Pollen | A Picea palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A Pinus palynomorph | |||
Unidentified [2] | Pollen | A pine family palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A Pseudolarix palynomorph | |||
Unidentified [2] | Pollen | A Tsuga palynomorph | |||
Unidentified [2] | Pollen | A Laricoidae palynomorph, similar to larch | |||
Unidentified [2] | Pollen | A Laricoidae palynomorph, similar to pseudotsuga | |||
Unidentified [2] | Pollen | A Platanus palynomorph | |||
Unidentified [2] | Pollen | A Potamogeton palynomorph | |||
Unidentified | Unidentified [2] | Pollen & macrofossils | Rose famnily palynomorphs | ||
Unidentified [2] | Pollen | A willow palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A duck weed palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A maple palynomorph | |||
Unidentified [2] | Pollen & macrofossils | A horse chestnut palynomorph | |||
Unidentified | Unidentified [2] | Pollen | A sapotaceous palynomorph | ||
Unidentified [2] | Pollen | A yew palynomorph | |||
Unidentified [2] | Pollen & macrofossils | An elm palynomorph | |||
Pollen | A palynomorph of uncertain affinity, possibly a Gentianaceae or Euphorbiaceae species | ||||
A group of six mosses were described from the Allenby Formation by Kuc (1972, 1974) representing the genera Ditrichites , Hypnites and Plagiopodopsis , with two species placed in the morphogenus Muscites . [10] [11] Dillhoff et al. (2013) identified twelve distinct gymnosperm taxa spanning the families Cupressaceae, Ginkgoaceae, and Pinaceae. While being the minority component of the Thomas Ranch flora by total fossil numbers, angiosperms have a higher diversity, with 45 distinct morphotypes represented as foliage, reproductive structures, or both. Seventeen of the morphotypes are identifiable to genus or species, with members of the family Betulaceae being most prominent. At least common one leaf type is suggested to possibly represent an extinct plant order, but has not been described. [2] Only two pteridophyte species have been described from the compression flora, Azolla primaeva by Penhallow (1890) and Equisetum similkamense by Dawson (1878). [12] [8]
The following fossil conifers, pteridophytes, ginkgophytes and bryophytes have been described from the Allenby Formation:
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
(Kuc) Miller | An amblystegiaceous moss | ||||
(Kuc) Miller | An amblystegiaceous moss | ||||
(Kuc) Miller | A bartramiaceous moss | ||||
Kuc | |||||
incertae sedis | † Muscites | Kuc | A moss of uncertain placement | ||
incertae sedis | † Muscites | Kuc | A moss of uncertain placement | ||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
A mosquito fern | |||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
A ginkgo | |||||
Mustoe, 2002 | A ginkgo with highly dissected leaves | ||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
(Lesquereux) MacGinitie | |||||
First identified as "Sequoia" brevifolia, "S." heeri. "S." langsdorfii (in part), "S." nordenskiöldi, & Taxodium distichum miocenum (in part) | |||||
Lesquereux | A redwood | ||||
First identified as "Sequoia" angustifolia, | |||||
Oldest true fir described | |||||
Undescribed [15] | A spruce | ||||
A pinaceous winged seed | |||||
Dawson, 1890 | |||||
(J.Nelson) Rehder | Originally identified as Pseudolarix americana, [15] then as Pseudolarix arnoldii [18] | ||||
Gooch | |||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Wolfe & Wehr | A sumac | ||||
Pigg, Bryan, & DeVore | An onion relative | ||||
(Berry) Wolfe & Wehr | An Alder | ||||
Wolfe & Wehr | A birch | ||||
Pigg, Manchester, & Wehr | A coryloid genus | ||||
(Dawson) Wolfe & Wehr | A katsura | ||||
† Fagopsis | (Knowlton) Wolfe & Wehr | A beech | |||
Undescribed [2] | A beech species Not described to species | ||||
Undescribed [2] | A gooseberry species | ||||
Radtke, Pigg & Wehr | A winter-hazel species | ||||
Undescribed [23] | A wingnut | ||||
Undescribed [23] | A laural species | ||||
Berry | A laural species | ||||
Undescribed [24] | An extinct sterculioid flower | ||||
† Tsukada | Wolfe & Wehr | A dove-tree relative | |||
Undescribed [2] | Manchester | A sycamore morphospecies | |||
(Lesquereux) Wolfe & Wehr | A sycamore | ||||
Unidentified [25] | A service berry | ||||
A snow wreath | |||||
A Sorbarieae genus | |||||
Wolfe & Tanai | A maple | ||||
Wolfe & Tanai | A maple | ||||
Wolfe & Tanai | A maple | ||||
Wolfe & Tanai | A maple | ||||
Wolfe & Tanai | A maple | ||||
Wolfe & Tanai | A maple | ||||
Wolfe & Tanai | A maple | ||||
McClain and Manchester | A Dipteronia species | ||||
Pigg et al. | A Tetracentron relative | ||||
Undescribed [2] | A trochodendraceous species | ||||
Denk & Dillhoff | An elm | ||||
Undescribed [5] | A nettle not described to genus | ||||
† Chaneya | (Lesquereux) Wang & Manchester | A sapindalean flower of uncertain affiliations | |||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
L.S. Russell, 1957 | A hydrobiid mud snail | ||||
L.S. Russell, 1957 | A lymnaeine pond snail | ||||
L.S. Russell, 1957 | An aplexine bladder snail | ||||
L.S. Russell, 1957 | A physine bladder snail | ||||
L.S. Russell, 1957 | An ancylinine ramshorn snail | ||||
Gyraulus ? | Indeterminate [32] | L.S. Russell, 1957 | A possible planorbinine ramshorn snail | ||
Indeterminate [32] | L.S. Russell, 1957 | A possible sphaeriine fingernail clam | |||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Unidentified | Unidentified [33] | A soldier beetle | |||
Unidentified | Unidentified [33] | A caraboid superfamily beetle | |||
Scudder, 1895 | |||||
Scudder, 1879 | |||||
Scudder, 1879 | |||||
Undescribed [34] | Scudder, 1895 | A click beetle | |||
Scudder, 1895 | |||||
Scudder, 1879 | |||||
Scudder, 1879 | |||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Rice, 1959 | A marchfly | ||||
Rice, 1959 | A marchfly | ||||
(Handlirsch, 1910) | A marchfly | ||||
(Handlirsh, 1910) | A marchfly | ||||
(Handlirsch, 1910) | A marchfly | ||||
(Handlirsch, 1910) | A marchfly | ||||
(Handlirsch, 1910) | A marchfly | ||||
Rice, 1959 | A marchfly | ||||
(Handlirsh, 1910) | A marchfly | ||||
(Handlirsh, 1910) | A marchfly Penthetria lambei (1910), Penthetria ovalis (1910), & Penthetria separanda (1910) considered junior synonyms (1959) | ||||
(Handlirsch, 1910) | A marchfly | ||||
(Handlirsh, 1910) | A marchfly | ||||
(Handlirsh, 1910) | A marchfly | ||||
(Scudder, 1879) | A marchfly | ||||
(Handlirsh, 1910) | A marchfly | ||||
Rice, 1959 | A marchfly | ||||
(Handlirsch, 1910) | A long-legged fly | ||||
Handlirsh, 1909 | |||||
(Handlirsh, 1910) | A cranefly | ||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Handlirsch, 1910 | |||||
Scudder, 1895 | |||||
Undescribed [40] | Scudder, 1895 | A spittlebug | |||
Scudder, 1895 | |||||
Scudder, 1895 | |||||
Scudder, 1879 | |||||
Scudder, 1895 | |||||
Scudder, 1895 | |||||
Undescribed [40] | Scudder, 1895 | A froghopper | |||
Scudder, 1895 | |||||
Scudder, 1895 | |||||
Scudder, 1879 | |||||
Undescribed [40] | Scudder, 1895 | A fulgorid plant hopper | |||
(Scudder, 1879) | A gerrine water strider | ||||
Scudder, 1879 | A hemipteran of uncertain placement | ||||
Archibald, Mathewes, & Aase (2023) reported a Titanomyrma species ant queen from the Vermillion Bluffs site, and noted the range extension for Formiciinae into the highlands, as the subfamily was previously considered a strictly thermophilic ant group. Due to complications arising from preservational distortion during diagenesis, they were unable to determine the correct size of the queen in life. If the distortion was lateral, then compression to bilateral symmetry yielded an adult length of approximately 3.3 cm (1.3 in), placing it the same range as Formicium berryi and F. brodiei , known only from wings, and sugg4ested as possible males. Conversely stretching the fossil to bilateral symmetry results in a larger 5 cm (2.0 in) length estimate, placing it as comparable to queens of T. lubei and T. simillima . [41]
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Undescribed [35] | A braconid wasp | ||||
Indeterminate [41] | A formiciine titan ant | ||||
(Handlirsch, 1910) | A xoridine ichneumon parasitic wasp | ||||
Rice, 1968 | |||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Archibald, 2005 | |||||
† Eomerope | Archibald & Rasnitsyn, 2018 | ||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
(Scudder, 1895) | A Polystoechotid-group giant lacewing [46] | ||||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Indeterminate | Indeterminate [47] | A daner dragonfly | |||
† Allenbya | Archibald & Cannings, 2022 | A possible Dysagrionidae odonate. | |||
Family | Genus | Species | Authority | Notes | Images |
---|---|---|---|---|---|
Archibald & Makarkin, 2021 | |||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Wilson, 1982 | A bowfin | ||||
Aves incertae sedis | Unidentified | Unidentified [50] | Mayr et al., 2019 | Indeterminate feathers and a skeleton | |
(Cope, 1893) | A catostomid sucker | ||||
† Trogosus | (Marsh, 1874) | A tillodont species | |||
(Hussakof, 1916) | A mooneye | ||||
Wilson, 1977 | A percopsiform fish | ||||
† Eosalmo | Wilson, 1977 | An ancestral salmon | |||
Undescribed [57] | A soft shelled turtle | ||||
The Princeton chert biota is unique in the Allenby formation due to the silicification of the chert, which has resulted in cellular and anatomical preservation of the organisms. As of 2016 over 30 different plant taxa had been described from chert fossils along with a number of fungal species. [58]
Order | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Currah, Stockey, LePage | An ascomycetan fungus on the host palm Uhlia allenbyensis | ||||
Klymiuk | An ascomycotan fungus | ||||
Currah, Stockey, LePage | An ascomycetan fungus on the host palm Uhlia allenbyensis | ||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Karafit et al. | |||||
Stockey, Nishida, & Rothwell | |||||
Smith et al. | |||||
Cevallos-Ferriz, Stockey, & Pigg | |||||
Undescribed [65] | An osmundaceous fern | ||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Bassinger | |||||
Stockey | A 2-needled Pine foliage | ||||
Stockey | A 3-needled Pine foliage | ||||
Miller | A basal Pine | ||||
Stockey | A pinaceous cone | ||||
Miller | A basal Pine | ||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Erwin & Stockey | An aquatic or emergent water-plantain | ||||
Grímsson, Zetter, & Halbritter | A Cape-pondweed pollen | ||||
Cevallos-Ferriz & Stockey | An arum family member | ||||
† Uhlia | Erwin & Stockey | ||||
Undescribed [74] | Cevallos-Ferriz | A current fruit | |||
Cevallos-Ferriz & Stockey | |||||
Cevallos-Ferriz & Stockey | A Liriodendron -like wood. | ||||
Pigg, Stockey & Maxwell | A Myrtaceous fruit | ||||
† Allenbya | Cevallos-Ferriz & Stockey | A water lily relative | |||
Stockey, LePage, & Pigg | A tuplo relative. | ||||
Bassinger | A rose family flower | ||||
Cevallos-Ferriz & Stockey | A prunoid wood. | ||||
"Species 1" [81] | Cevallos-Ferriz & Stockey | A prunoid seed. | |||
"Species 2" [81] | Cevallos-Ferriz & Stockey | A prunoid seed. | |||
"Species 3" [81] | Cevallos-Ferriz & Stockey | A prunoid seed. | |||
Erwin & Stockey | A possible dodonaecous soapberry family flower | ||||
Smith & Stockey | A lizard's-tail species | ||||
Cevallos-Ferriz & Stockey | A grape family fruit of uncertain generic placement [85] | ||||
incertae sedis | "Type 1" [84] | Cevallos-Ferriz & Stockey | A grape family fruit of uncertain generic placement | ||
incertae sedis | "Type 2" [84] | Cevallos-Ferriz & Stockey | A grape family fruit of uncertain generic placement | ||
Zetter & Hesse | A possible iridaceous pollen morphotype | ||||
† Eorhiza | Robison & Person | A semi-aquatic dicot of uncertain affinity. | |||
† Ethela | Erwin & Stockey | A cyperaceous or juncaceous monocot | |||
Stockey | A possibly aquatic magnoliopsid flower of uncertain affiliation. | ||||
Erwin & Stockey | A lilialean genus of uncertain placement | ||||
Driftwood Canyon Provincial Park is a provincial park in British Columbia, Canada. Driftwood Canyon Provincial Park covers 23 ha of the Bulkley River Valley, on the east side of Driftwood Creek, a tributary of the Bulkley River, 10 km northeast of the town of Smithers. The park is accessible from Driftwood Road from Provincial Highway 16. It was created in 1967 by the donation of the land by the late Gordon Harvey (1913–1976) to protect fossil beds on the east side of Driftwood Creek. The beds were discovered around the beginning of the 20th century. The park lands are part of the asserted traditional territory of the Wet'suwet'en First Nation.
Lasioideae is a subfamily of flowering plants in the family Araceae. It contains ten living genera: Anaphyllopsis, Anaphyllum, Cyrtosperma, Dracontioides, Dracontium, Lasia, Lasimorpha, Podolasia, Pycnospatha, and Urospatha. The subfamily also includes the extinct genus Keratospema described from Ypresian fossils recovered at the Eocene Okanagan Highlands Princeton Chert site.
Azolla primaeva is an extinct species of "water fern" in the family Salviniaceae known from Eocene fossils from the Ypresian stage, found in southern British Columbia.
Decodon verticillatus, the sole living species in the genus Decodon, is a flowering plant in the family Lythraceae. It is commonly known as waterwillow or swamp loosestrife. It is native to wetlands in the eastern half of the United States and Canada.
Neviusia dunthornei is an extinct species of flowering plants in the family Rosaceae. The species is solely known from the early Eocene, Ypresian stage, Allenby Formation Lacustrine deposits near the town of Princeton, British Columbia.
The Princeton Chert is a fossil locality in British Columbia, Canada, which comprises an anatomically preserved flora of Eocene Epoch age, with rich species abundance and diversity. It is located in exposures of the Allenby Formation on the east bank of the Similkameen River, 8.5 km (5.3 mi) south of the town of Princeton, British Columbia.
The McAbee Fossil Beds is a Heritage Site that protects an Eocene Epoch fossil locality east of Cache Creek, British Columbia, Canada, just north of and visible from Provincial Highway 97 / the Trans-Canada Highway. The McAbee Fossil Beds, comprising 548.23 hectares, were officially designated a Provincial Heritage Site under British Columbia's Heritage Conservation Act on July 19, 2012. The site is part of an old lake bed which was deposited about 52 million years ago and is internationally recognised for the diversity of plant, insect, and fish fossils found there. Similar fossil beds in Eocene lake sediments, also known for their well preserved plant, insect and fish fossils, are found at Driftwood Canyon Provincial Park near Smithers in northern British Columbia, on the Horsefly River near Quesnel in central British Columbia, and at Republic in Washington, United States. The Princeton Chert fossil beds in southern British Columbia are also Eocene, but primarily preserve an aquatic plant community. A 2016 review of the early Eocene fossil sites from the interior of British Columbia discusses the history of paleobotanical research at McAbee, the Princeton Chert, Driftwood Canyon, and related Eocene fossil sites such as at Republic.
Nuphar carlquistii is an extinct species of flowering plant in the family Nymphaeaceae related to the modern spatterdock, Nuphar advena. The species is known from fossil seeds and fruits found in the early Eocene Okanagan Highlands deposits of northern Washington state and British Columbia, Canada.
Betula leopoldae is an extinct species of birch in the family Betulaceae. The species is known from fossil leaves, catkins, and inflorescences found in the early Eocene deposits of northern Washington state, United States, and similar aged formations in British Columbia, Canada. The species is placed as basal in Betula, either as a stem group species, or an early divergent species.
Tetracentron hopkinsii is an extinct species of flowering plant in the family Trochodendraceae. The species is known from fossil leaves found in the early Eocene deposits of northern Washington state, United States and south Central British Columbia. The species was first described from fossil leaves found in the Allenby Formation. T. hopkinsii are possibly the leaves belonging to the extinct trochodendraceous fruits Pentacentron sternhartae.
The paleoflora of the Eocene Okanagan Highlands includes all plant and fungi fossils preserved in the Eocene Okanagan Highlands Lagerstätten. The highlands are a series of Early Eocene geological formations which span an 1,000 km (620 mi) transect of British Columbia, Canada and Washington state, United States and are known for the diverse and detailed plant fossils which represent an upland temperate ecosystem immediately after the Paleocene-Eocene thermal maximum, and before the increased cooling of the middle and late Eocene to Oligocene. The fossiliferous deposits of the region were noted as early as 1873, with small amounts of systematic work happening in the 1880-90s on British Columbian sites, and 1920-30s for Washington sites. A returned focus and more detailed descriptive work on the Okanagan Highlands sites revived in the 1970's. The noted richness of agricultural plant families in Republic and Princeton floras resulted in the term "Eocene orchards" being used for the paleofloras.
Fagus langevinii is an extinct species of beech in the family Fagaceae. The species is known from fossil fruits, nuts, pollen, and leaves found in the early Eocene deposits of South central British Columbia, and northern Washington state, United States.
The Eocene Okanagan Highlands or Eocene Okanogan Highlands are a series of Early Eocene geological formations which span a 1,000 km (620 mi) transect of British Columbia, Canada, and Washington state, United States. Known for a highly diverse and detailed plant and animal paleobiota the paleolake beds as a whole are considered one of the great Canadian Lagerstätten. The paleobiota represented are of an upland subtropical to temperate ecosystem series immediately after the Paleocene–Eocene thermal maximum, and before the increased cooling of the middle and late Eocene to Oligocene. The fossiliferous deposits of the region were noted as early as 1873, with small amounts of systematic work happening in the 1870–1920s on British Columbian sites, and 1920–1930s for Washington sites. Focus and more detailed descriptive work on the Okanagan Highland sites started in the late 1960s.
The paleofauna of the Eocene Okanagan Highlands consists of Early Eocene arthropods, vertebrates, plus rare nematodes and molluscs found in geological formations of the northwestern North American Eocene Okanagan Highlands. The highlands lake bed series' as a whole are considered one of the great Canadian Lagerstätten. The paleofauna represents that of a late Ypresian upland temperate ecosystem immediately after the Paleocene-Eocene thermal maximum, and before the increased cooling of the middle and late Eocene to Oligocene. The fossiliferous deposits of the region were noted as early as 1873, with small amounts of systematic work happening in the 1880-90s on British Columbian sites, and 1920-30s for Washington sites. Focus and more detailed descriptive work on the Okanagan Highlands site started in the last 1970's. Most of the highlands sites are preserved as compression-impression fossils in "shales", but also includes a rare permineralized biota and an amber biota.
Uhlia is an extinct genus of coryphoid palm containing a single species Uhlia allenbyensis. The species is known from permineralized remains recovered from the Princeton Chert in British Columbia, Canada. Leaves of Uhlia have "tar spot"-like fungal infections of the extinct ascomycete Paleoserenomyces, which in turn are hyperparasitized by the ascomycete Cryptodidymosphaerites.
Paleoserenomyces is an extinct monotypic genus of pleosporale fungus of uncertain family placement. When described it contained the single species Paleoserenomyces allenbyensis. The genus is solely known from the Early Eocene, Ypresian aged, Princeton Chert deposit of the Allenby Formation. Palaeoserenomyces is one of only three described fossil fungus species found in the Princeton Chert, being a tar spot like parasite of the fossil palm Uhlia allenbyensis, and is host for the hyperparasite Cryptodidymosphaerites princetonensis.
Cryptodidymosphaerites is an extinct monotypic genus of pleosporale fungus of uncertain family placement. When described it contained the single species Cryptodidymosphaerites princetonensis. The genus is solely known from the Early Eocene, Ypresian aged, Princeton Chert deposit of the Allenby Formation. Cryptodidymosphaerites is one of only three described fossil fungus species found in the Princeton Chert, and is a hyperparasite of Palaeoserenomyces allenbyensis, itself a tar spot-like parasite of the fossil palm Uhlia.
Dickwhitea is an extinct morphogenus of lady fern containing a single morphospecies Dickwhitea allenbyensis. The species is known from permineralized remains recovered from the Princeton Chert in British Columbia, Canada. Rhizomes of Dickwhitea are noted for having a sympodial vascular architecture notably similar to Ginkgo biloba and Sequoia sempervirens.
The Paleobiota of the Klondike Mountain Formation comprises a diverse suite of Early Eocene plants and animals recovered from North Central Washington State. The formation outcrops in locations across the north western area of Ferry County, with major sites in Republic, north west of Curlew Lake, and on the Toroda Creek area. The formation is the southern most of the Eocene Okanagan Highlands, sharing much of the paleoflora and paleofauna with site across Central and southern British Columbia.
Allenbya is an extinct genus of water lilies in the family Nymphaeaceae containing a single species Allenbya collinsonae. The species is known from permineralized remains recovered from the Early Eocene Princeton Chert in British Columbia, Canada.