The Paleobiota of the Klondike Mountain Formation comprises a diverse suite of Early Eocene plants and animals recovered in North Central Washington State from the Klondike Mountain Formation. 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.
Dillhoff et al. (2013) reference undescribed moss specimens known from the Klondike Mountain Formation known from vegetative gametophytes and they noted them to be similar to undescribed specimens from the Allenby Formation and Horsefly shales. [1]
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Undescribed | Undescribed | Undescribed [1] | Undescribed moss specimens | |||
Rare specimens of Selaginella fossils were noted by Wehr (1998), with no species level description. [2]
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Undescribed [2] | A spikemoss | |||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Undescribed [2] | A possible bladder fern relative | ||||
Pigg et al. | |||||
A scouring rush | |||||
Pigg et al. | |||||
A climbing fern | |||||
Undescribed [7] | A "watermoss" species. | ||||
Three major groups of gymnosperms are present in the Klondike Mountain Formation, with the most speciose being the pinophytes. The ginkgophytes are represented by two species of Ginkgo , while an undescribed Zamiaceae member is the sole cycadophyte.
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Undescribed | A zamiaceous cycad. | ||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Ginkgoaceae | Ginkgo | A ginkgo | |||
A ginkgo | |||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Cupressaceae | An incense cedar | ||||
A false cypress | |||||
A sugi | |||||
Undescribed [12] | A Chinese swamp cypress | ||||
A coast redwood | |||||
Undescribed [7] | A Taiwania species | ||||
(Sternberg) Heer | |||||
An arborvitae | |||||
Undescribed [13] | A possible Thujopsis | ||||
Pinaceae | Oldest true fir described | ||||
Undescribed [12] | A spruce | ||||
Pinus | Berry | A 5-needle pine | |||
Berry | A 3-needle pine, jr homonym to Pinus macrophylla Lindley 1839 | ||||
Berry | A pine seed morphogenus | ||||
Berry | A purported 4-needle pine | ||||
Gooch | A golden larch | ||||
Undescribed [12] | A hemlock | ||||
Undescribed [12] | An umbrella pine | ||||
Taxaceae | A yew | ||||
Undescribed [12] | A yew | ||||
Undescribed [12] | A yew | ||||
A plum-yew relative | |||||
Angiosperms, commonly called flowering plants belong to a single plant clade which diverged from other plants during the prior to the Cretaceous, and began to rapidly evolve and radiate by the Middle Cretaceous. [21] Angiosperm diversification during the Cretaceous and Paleocene resulted in eight recognized clades that are segregated into two groups the Basal angiosperms and Core angiosperms. Present in the Klondike Mountain Formation are four of the eight groups, Nymphaeales representing Basal Angiosperms, plus Magnoliids, Monocots, and Eudicots all in the Core angiosperms.
The Basal Angiosperms are represented by a single Nymphaeales water-lily species Nuphar carlquistii , [22] though a second member, Allenbya collinsonae , has been described from the Princeton Chert. [23] Wehr (1995) illustrated two fossils that were tentatively identified as fruits of the banana genus Ensete and the extinct myrtle genus Paleomyrtinaea respectively, [24] however further fossil finds resulted in the re-identification of the first as a N. carlquistii rhizome section, and the second is a seed mass from the same water-lily. [22]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
DeVore, Taylor, & Pigg | A waterlily, | ||||
Under the APG IV system of flowering plant classification, the magnoliids are divided into four orders Canellales, Laurales, Magnoliales, and Piperales. Member species and undescribed taxa placed confidently in the Laurales and Magnoliales are present in the formation. The laurales are the most diverse magnoliid order of the formation with one described species Sassafras hesperia plus three tentatively identified genera which have not been described. Of the magnoliales, only an undescribed Magnolia , having possible affinity with Magnolia subg. Talauma , is found in the formation, while Liriodendroxylon princetonensis has described from permineralized wood in the Princeton Chert. [25] The extinct angiosperm genus Dillhoffia has noted similarities to the piperalean family Aristolochiaceae, but was left incertae sedis as to family by Manchester and Pigg (2008) due to a lack of confident morphological characters for placement. Piperales are known from the Princeton chert, with Saururus tuckerae representing the oldest confident Saururaceae species in the fossil record. [26]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Lauraceae | Undescribed [2] | A lauraceous form species. | |||
Undescribed [2] | A stinkwood species. | ||||
Undescribed [16] | A Phoebe species. | ||||
Undescribed [27] | A magnolia, possibly Magnolia subgenus Talauma | ||||
Manchester & Pigg | A flower of uncertain floral affinity | ||||
The second largest clade of flowering plants, monocots are divided into eleven separate orders and of those, the Alismatales, Asparagales, Liliales, and Poales are found in the Klondike Mountain Formation, each represented by a single taxon. The Alismatales are represented by the Araceae species Orontium wolfei , which is considered similar to the modern golden clubs of eastern North America, while the extinct Paleoallium belongs to the Liliales. Asparagales and Poales are both present as undescribed species associated with the genera Smilax and Typha respectively. Extinct genera of monocots are also represented in the Princeton chert by the arecalean palm Uhlia , [29] the alismatalean genus Heleophyton , [30] the alismatalean Keratosperma , [31] the asparagalean pollen morphogenus Pararisteapollis , [32] the lilialean genus Soleredera , [33] and the poalean genus Ethela , [34]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Pigg, Bryan, & DeVore | An onion relative | ||||
Undescribed [2] | A greenbrier species. | ||||
Undescribed [2] | A cattail species. | ||||
Over a dozen different Rosaceae genera, both extant and extinct, have been identified in the formation providing some of the oldest reliable macrofossil records (excluding fossil pollen) for the family. [37] Benedict et al. (2011) described first fossils for the prunoid genus Oemleria along with the oldest Prunus flowers. The Prunus flowers are complemented by leaf fossils representing five to six distinct morphotypes. [38] Spiraea is known from an inflorescence with multiple flowers and leaves that are either from the genus or a closely related extinct type. The leaves frequently are preserved with a persistent stipule, a feature not found in modern Spiraea species. The firethorn genus Pyracantha and the South American genus Hesperomeles have been tentatively identified from leaves while Maloidea leaves belonging to either Malus or Pyrus have been found. Two distinct species of the Asian endemic genus Photinia are known, however only one of them Photinia pagae had been described as of 2007. [38] The rosaceous genus Physocarpus had been reported by Hopkins and Wehr (1994) as also occurring in the formation, [27] however subsequent examination of the fossils by Oh & Potter (2005) failed to find stellate trichomes which are a distinct feature of the genus. They noted the fossils might be stem Neillieae, the rose tribe containing both Physocarpus and Neillia , or possibly Rubus , Crataegus , or Ribes . [39]
Fossils of both Sorbus and Rhus species leaves showing evidence of being interspecies hybrids have been noted from the formation and Flynn, DeVore and Pigg (2019) described four species of sumac which formed multiple hybrids. [40] Between three and four Trochodendraceae species that have been described from the Klondike Mountain Formation. Broadly circumscribed four species in three genera have been identified at Republic, Paraconcavistylon wehrii , Pentacentron sternhartae , Tetracentron hopkinsii , and Trochodendron nastae . Additionally the species Trochodendron drachukii is known from related Kamloops group shales at the McAbee Fossil Beds near Cache Creek, British Columbia. Manchester et al. 2018 noted that Tr. drachukii is likely the fruits of Tr. nastae, while Pe. sternhartae are likely the fruits of Te. hopkinsii. [41] If fossils of the fruits and foliage in attachment are found, that would bring the species count down to three whole plant taxa. [41] Additionally, the extinct genus Nordenskioldia is also known from the formation. The placement of Nordenskioldia is debated, with some treatments placing it into Trochodendraceae, while a 2020 analysis placed it outside of the crown-group Trochodendaceae. [42] Wesley Wehr in 1994 reported Bignoniaceae seeds along with a single Rubiaceae fruit and an isolated Fabaceae leaf. [43] An update of the floral list by Wehr and Manchester published in 1996 added an additional fifteen taxa identified from reproductive structures such as flowers fruits or seeds. [24]
Pigg, Manchester, and Wehr (2003) noted in during the description of Corylus johnsonii and Carpinus perryae that they were the oldest confirmed hazelnut and hornbeam fossils. [44] That status was affirmed by Forest et al. (2005) who used both as fossil calibration points for phylogenetic analysis of Betulaceae. [45] Within the family Bignoniaceae, the fossil seeds and fruits are noted by Ze-Long Nie et al (2006) as the oldest confirmed for the family. [46]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Anacardiaceae | Rhus | Flynn, DeVore, & Pigg | A sumac, | ||
Flynn, DeVore, & Pigg | A sumac, | ||||
(Wolfe and Wehr) Flynn, DeVore & Pigg | A sumac, | ||||
Flynn, DeVore, & Pigg | A sumac, | ||||
Undescribed [5] | A holly | ||||
Undescribed [9] | A spikenard species | ||||
Betulaceae | (Berry) Wolfe & Wehr | An Alder | |||
Wolfe & Wehr | A birch | ||||
Pigg, Manchester, & Wehr | A hornbeam | ||||
Pigg, Manchester, & Wehr | |||||
† Palaeocarpinus | Pigg, Manchester, & Wehr | A birch relative | |||
Undescribed [44] | A birch relative | ||||
Undescribed | Undescribed [43] | A catalpa family member | |||
Wolfe & Wehr | An extinct Bursera relative | ||||
Undescribed [48] | A cannabaceous fruit | ||||
(Dawson) Wolfe & Wehr | A katsura with suggested affinity to † Joffrea , [9] | ||||
A dogwood species, | |||||
Undescribed [48] | An elaeocarpaceous fruit | ||||
Ericaceae | A madrone relative | ||||
A rhododendron | |||||
Undescribed [27] | A doghobble relative | ||||
A "hard rubber tree" | |||||
Fagaceae | Undescribed [5] | A Castanea relative | |||
† Fagopsis | (Knowlton) Wolfe & Wehr | A beech relative | |||
Manchester & Dillhoff | A beech | ||||
An oak | |||||
Grossulariaceae | Ribes | A current | |||
"Species2" [27] | A current | ||||
Hamamelidaceae | |||||
Radtke, Pigg, & Wehr | |||||
Hydrangeaceae | Undescribed [27] | A Hydrangea. | |||
Undescribed [27] | A mock-orange | ||||
A Phytocrene relative | |||||
A virginia willow species | |||||
Juglandaceae | A walnut family relative. | ||||
(Brown) Manchester | A walnut family relative. | ||||
A walnut family relative. | |||||
Undescribed [43] | A wing nut | ||||
Undescribed [9] | A swamp loosestrife | ||||
Malvaceae | Undescribed [43] | A Craigia species | |||
A chocolate relative | |||||
Undescribed [27] | A hibiscus | ||||
Undescribed [43] | A linden relative | ||||
Wolfe & Wehr | A Linden | ||||
Undescribed [48] | Linden relative fruits | ||||
(LaMotte) Wolfe & Wehr | First described as a dogwood under "Cornus acuminata | ||||
Undescribed [24] | A moonseed | ||||
Undescribed [27] | A mulberry, two types known. | ||||
Dawson | |||||
† Tsukada | Wolfe & Wehr | A dove-tree relative | |||
Undescribed [9] | A leaf morphotype of uncertain affiliation. | ||||
Platanaceae | Huegele & Manchester | A plane tree fruit taxon affiliated with Langeria | |||
† Langeria | Wolfe & Wehr | A plane tree | |||
Undescribed [43] | Manchester | A plane tree fruit taxon | |||
(Lesquereux) Wolfe & Wehr | A plane tree relative | ||||
Undescribed [48] | A sycamore stamen head | ||||
† Deviacer | Undescribed [43] | A milkwort relative | |||
Undescribed [27] | A Clematis | ||||
Rosaceae | Undescribed [27] | A service berry | |||
Undescribed [27] | A hawthorn relative | ||||
Undescribed [5] | An apple | ||||
Undescribed [38] | A maloid species possibly apple or pear | ||||
Undescribed [27] | A snow-wreath | ||||
Benedict, DeVore, & Pigg | An Osoberry | ||||
Wolfe & Wehr | A Christmas-berry relative | ||||
Undescribed [9] | A possible nine-bark | ||||
Prunus | Benedict, DeVore, & Pigg | A cherry relative | |||
"Species 1" [16] | A prunoid leaf | ||||
"Species 2" [16] | A prunoid leaf | ||||
"Species 3" [16] | A prunoid leaf | ||||
Undescribed [38] | A firethorn sp. [38] | ||||
Undescribed [38] | A maloid species possibly apple or pear | ||||
Undescribed [27] | A blackberry | ||||
A rowan relative | |||||
A bridal wreath | |||||
Undescribed [38] | A bridal wreath relative | ||||
Sabiaceae | Undescribed [24] | A Meliosma species | |||
Undescribed [24] | A Sabia species | ||||
Salicaceae | A cottonwood | ||||
Undescribed [9] | A willow relative | ||||
A willow | |||||
Sapindaceae | Acer ? | Heer, 1876 | A possible maple | ||
Acer | 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 | ||||
A horse chestnut | |||||
Becker | A sapindaceous species | ||||
† Bohlenia | (Brown) Wolf & Wehr | An extinct sapindalean species | |||
Wang et al. | A Koelreuteria species | ||||
Undescribed [2] | A kadsura species. | ||||
Theaceae | "Species A" [16] | A theaceous species similar to Gordonia | |||
"Species B" [16] | A theaceous species similar to Cleyera | ||||
Undescribed [43] | A trochodendroid of uncertain placement. [42] | ||||
Trochodendraceae | (Manchester et al.) | A Trochodendrale | |||
Manchester et al. | |||||
Pigg et al. | A Trochodendrale, | ||||
Pigg, Wehr, & Ickert-Bond | A Trochodendron | ||||
Undescribed [9] | A trochodendroid of uncertain placement. [42] | ||||
Ulmaceae | Undescribed [24] | An elm relative | |||
Ulmus | (Berry) LaMotte | An elm species | |||
Denk & Dillhoff | An elm species, | ||||
Incertae sedis | Crane | A winged fruit of unidentified affinities | |||
Smith, Greenwalt & Manchester | A samara of uncertain affiliation. | ||||
Manchester | A samara of uncertain affinities. | ||||
Wolfe & Wehr | An incertae sedis angiosperm | ||||
The insect fauna of the Klondike Mountain Formation includes representatives from over 13 orders, based on a 1992 estimate, including immature though adult specimens and both terrestrial and aquatic taxa. [65] The most prevalent orders are Diptera and Hemiptera, each making up approximately 30% of the fossil insects known in 1992.
Family | Genus | species | Authors | Notes | Images |
---|---|---|---|---|---|
Undescribed | Undescribed [5] | A Diplopterine cockroach | |||
Undescribed | Undescribed [65] | A blattoidean cockroach | |||
Undescribed | Undescribed [65] | Undescribed termites of uncertain affiliation | |||
A list of Coleopteran families identified by 1992 included Carabidae, Cerambycidae, Chrysomelidae, Curculionidae, Dytiscidae, Elateridae and Lucanidae, [65] but the beetle fauna has not been described in depth yet, with only two weevil species having been fully described. [66] [67] A third beetle group belonging to the bean beetle tribe Pachymerini has been identified as palm beetles of the Caryobruchus – Speciomerus genus group. [68]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Brentidae | Legalov, 2013 | ||||
Legalov, 2015 | |||||
Undescribed | Undescribed [65] | A ground beetle | |||
Undescribed | Undescribed [65] | A long-horn beetle | |||
Caryobruchus – Speciomerus genus group | Undescribed [68] | palm beetles in the tribe Pachymerini. | |||
Undescribed | Undescribed [65] | A diving beetle | |||
Undescribed | Undescribed [65] | A click beetle | |||
Undescribed | Undescribed [65] | A stag beetle | |||
Unidentified | Undescribed | Undescribed [69] | A possible staphylinoid beetle | ||
The order Dermaptera was first reported in 1992 [65] and is known from a series of isolated partial specimens, mostly abdominal sections with the distinct anal forceps attached. Based on the forceps structuring the specimens were tentatively assigned to the modern family Forficulidae, as the oldest North American representatives of the family known at that time. [70]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Forficulidae? | Unidentified | "Forficulid species 1" [70] | A possible forficulid earwig with long cerci | ||
"Forficulid species 2" [70] | A possible forficulid earwig with short cerci | ||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Undescribed | Undescribed [65] | A march fly | |||
Undescribed | Undescribed [71] | Trace fossils | |||
Undescribed | Undescribed [69] | A dagger fly | |||
Undescribed | Undescribed [65] | A fungus gnat | |||
A pipunculid big-headed fly | |||||
Unidentified | Unidentified [73] | A hover fly | |||
Undescribed | Undescribed [65] | A crane fly | |||
Lewis (1992) listed one species of Heptageniidae and three specimens that he did not place to family. [65] The next year Lewis and Wehr (1993) gave a slightly more detailed description of the specimens again identifying one to Heptageniidae, possibly in the genera Heptagenia or Stenonema . [74] The specimens were later examined by Nina D. Sinitchenkova (1999) who described one as a squaregill mayfly and the oldest member of the genus Neoephemera , confirmed the Heptageniidae identification but that it was unidentifiable to genus. The last specimen she confirmed as an ephemeropteran, but unidentifiable below order level. [75]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Indeterminate | Indeterminate [65] | A flat headed mayfly nymph. | |||
Sinitchenkova, 1999 | |||||
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Undescribed | Undescribed [65] | An aphid | |||
Aphrophoridae | Undescribed [65] | An aphrophorid spittlebug | |||
Undescribed [65] | An aphrophorid spittlebug | ||||
Cercopidae | Undescribed [65] | A cercopid froghopper | |||
Undescribed | Undescribed [65] | A cercopid froghopper | |||
Undescribed | Undescribed [65] | A frog hopper | |||
Undescribed | Undescribed [65] | A Shield or stink bug | |||
A review of the Okanagan highlands hymenoptera published in 2018 identified four "Symphyta" families in the formation Cimbicidae, Pamphiliidae, Siricidae, and Tenthredinidae. Of the "Apocrita" families thirteen are represented, the "Parasitica" families are Braconidae, Diapriidae Ichneumonidae, Proctotrupidae, and Roproniidae while the Vespoidea families are Formicidae, Pompilidae, Scoliidae and Vespidae. Within Apoidea the "Spheciformes" families include Angarosphecidae and Sphecidae while Halictidae is the sole "Apiformes" family known from body fossils. Prunus and Ulmus leaves have been found having damage that is consistent with the damage pattern left by Megachilidae species bees when they remove sections of tissue for nest lining. There are several additional Apoidea fossils that were left as incertae sedis in the group based on the similarity between them and Paleorhopalosoma menatensis , a Paleocene species described from the Menat Formation Auvergne, France. The placement of P. menatensis is uncertain, having been initially described as a member of Rhopalosomatidae, but is possibly an Angarosphecidae or closely related taxon, based on the wing and body morphology. [76]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Angarosphecidae | Undescribed [76] | An angarosphecid spheciform wasp. | |||
Undescribed | Undescribed [76] | An angarosphecid spheciform wasp | |||
Undescribed | braconid parasitic wasps | ||||
Cimbicidae | † Leptostigma [77] | Archibald & Rasnitsyn, 2023 | |||
Archibald & Rasnitsyn, 2023 | A cenocimbicine cimbicid sawfly | ||||
Undescribed | Undescribed [71] | Trace fossils | |||
Undescribed | Undescribed [76] | A diapriid diaprioid wasp | |||
Formicidae | Dlussky & Rasnitsyn, 2003 | An ant of uncertain subfamily affiliation | |||
"Indesterminate" [79] | |||||
(Dlussky & Rasnitsyn, 1999) | An ant, described as Camponotites kraussei, | ||||
Dlussky & Rasnitsyn, 1999 | A bulldog ant, first described as a Rhopalosomatidae wasp, | ||||
Undescribed | Undescribed [76] | Ants of uncertain subfamily placement. [76] | |||
Halictidae (?) | Undescribed | Undescribed [76] | A possible sweat bee | ||
Undescribed | Undescribed [76] | ichneumonid parasitic wasps unplaced to subfamily | |||
Undescribed | Undescribed [76] | Megachilid leaf-cutter bee herbivory trace fossils on leaves | |||
Archibald & Rasnitsyn, 2015 | A parasitic wasp | ||||
Undescribed | Undescribed [76] | A pompilid spider wasp | |||
Undescribed | Undescribed [76] | A proctotrupid parasitic wasp | |||
Undescribed | Undescribed [76] | A roproniid (sensu lato) proctotrupoid wasp | |||
Archibald & Rasnitsyn, 2022 | |||||
Undescribed | Undescribed [76] | An archaeoscoliine scoliid wasps | |||
Undescribed | Undescribed [76] | A sphecid (sensu stricto) wasp | |||
Undescribed | Undescribed [76] | A Tenthredinid sawfly | |||
Undescribed | Undescribed [76] | A vespid wasp | |||
A solitary lepidopteran body fossil has been recovered, but no full descriptive work has been made on the specimen, aside from a single PhD dissertation. Early examination placed the moth in the family Geometridae, but later work has identified it as the oldest member of the tiger moth subfamily Arctiinae. [85] Trace fossil evidence from leaf fossil herbivory indicates at least four other possible lepidopteran families were present in the formation.
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
Undescribed | Undescribed [71] | Trace fossils | |||
Undescribed | Undescribed [85] | An arctiine tiger moth | |||
Undescribed | Trace fossils | ||||
Undescribed [71] | Trace fossils | ||||
Undescribed [71] | Trace fossils | ||||
A number of mecopteran species belonging to the families Cimbrophlebiidae, Dinopanorpidae, Eorpidae, and Panorpidae are also known. [87]
Family | Genus | Species | Authors | Notes | Images |
---|---|---|---|---|---|
†Cimbrophlebiidae | † Cimbrophlebia | Archibald, 2009 | |||
Archibald, 2009 | |||||
†Dinopanorpidae | † Dinokanaga | Archibald, 2005 | A scorpion fly species | ||
Archibald, 2005 | A scorpion fly species | ||||
Archibald, 2005 | A scorpion fly species | ||||
†Eorpidae | † Eorpa | Archibald, Mathewes, & Greenwood, 2013 | A mecopteran scorpionfly | ||
Archibald, Mathewes, & Greenwood, 2013 | A mecopteran scorpionfly, tentatively identified | ||||
Undescribed | Undescribed [89] | Undescribed common scorpionflies | |||
The neuropteran insects (lacewings and their allies) identified as of 2014 include species from the families Berothidae, Chrysopidae, Hemerobiidae, Ithonidae (including Polystoechotidae), Nymphidae, Osmylidae, and Psychopsidae. [90]
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
2013 | ||||||
(Makarkin, Archibald, & Oswald, 2003) | 2003 | A hemerobiid lacewing | ||||
Ithonidae | Makarkin & Archibald, 2009 | 2009 | ||||
† Palaeopsychops | Archibald & Makarkin, 2006 | 2006 | A polystechotid group [97] moth lacewing | |||
Archibald & Makarkin, 2006 | 2006 | A polystechotid group [97] moth lacewing | ||||
† Polystoechotites | Archibald & Makarkin, 2006 | 2006 | A polystechotid group [97] moth lacewing | |||
Archibald & Makarkin, 2006 | 2006 | A polystechotid group [97] moth lacewing | ||||
Archibald & Makarkin, 2006 | 2006 | A polystechotid group [97] moth lacewing | ||||
? Nymphes | Archibald, Makarkin, & Ansorge, 2009 | 2009 | A nymphid lacewing, possibly a species of † Epinesydrion [99] | |||
Makarkin, Archibald, & Mathewes, 2021 | 2021 | |||||
Makarkin & Archibald, 2014 | 2014 | A possible psychopsid lacewing | ||||
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Aeshnidae | Archibald & Cannings, 2019 | 2019 | ||||
Archibald & Cannings, 2019 | 2019 | |||||
† Ypshna | Archibald & Cannings, 2019 | 2019 | ||||
†Dysagrionidae | Archibald & Cannings, 2021 | 2021 | ||||
Archibald & Cannings, 2021 | 2021 | |||||
† Okanagrion | Archibald & Cannings, 2021 | 2021 | ||||
Archibald & Cannings, 2021 | 2021 | |||||
Archibald & Cannings, 2021 | 2021 | |||||
Archibald & Cannings, 2021 | 2021 | |||||
Archibald & Cannings, 2021 | 2021 | |||||
Archibald & Cannings, 2021 | 2021 | |||||
Archibald & Cannings, 2021 | 2021 | |||||
Archibald & Cannings, 2021 | 2021 | A gossamerwing damselfly. | ||||
Archibald & Cannings | 2021 | |||||
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Archibald, Gu, & Mathewes | 2022 | A grasshopper/hump-back grig relative | ||||
Fossil wings first described in 2015 were identified as being from Susumanioidea stick-insects, a group that had previously been known from the Jurassic to the Paleocene only. [105] Archibald and Bradler (2015) did not place Eoprephasma into Susumaniidae family, maintaining that known characters of the describe specimens did not match taxa in the family, they instead kept the genus as Susumanioidea incertae sedis. Phylogenetic analysis of Susumanioidea published by Yang et al. (2021) resulted in placement of Eoprephasma as the sister group to Renphasma deep within the Susumaniidae subfamily Susumaniinae. The phylogeny produced by Yang et al. indicated a sister group state with the Cretaceous genus Renphasma of China, and placed both as the most derived of the Susumaniinae taxa. [106]
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Archibald & Bradler, 2015 | 2015 | A Susumaniinae stick insect species | ||||
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Archibald & Makarkin, 2021 | 2021 | |||||
Trichopterans are known mainly from laraval cases and occasional isolated wings. [108]
Family | Genus | species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Unidentified | giant caddisflies | |||||
Unidentified | unidentified [65] | northern caddisflies | ||||
Five species of fish have been identified from the formation, four of which are known from skeletal elements, while the fifth is only known from isolated scales. [109] Of the five species, two are unique to the formation, Hiodon woodruffi and Libotonius pearsoni were both described by paleoichthyologist Mark V. H. Wilson in 1978 and 1979 respectively. The other three species, "Amia" hesperia , Amyzon aggregatum , and Eosalmo driftwoodensis , were first described from Okanagan Highlands formations in British Columbia and subsequently also identified from Ferry County fossils. The first notation of fish fossils in the Republic area was by Joseph Umpleby in his 1910 visit to the area, who collected fish near the Tom Thumb Mine, and sent them to the National Museum of Natural History. After examining the fossils, Charles R. Eastman listed the specimens as belonging to the extinct species Amyzon brevipinne in his Fossil fishes in the collection of the United States National Museum. [110] Research tapered off until a series of fish were collected in the Toroda Creek Graben northwest of Republic by Robert Carl Pearson during his early 1960's field mapping for the Geologic map of the Bodie Mountain quadrangle, Ferry and Okanogan Counties, Washington. The fossils were tentatively identified by paleoichthyologist David Dunkle in 1962 and 1965 as members of the genera Amyzon , Tricophanes , Erismatopterus and an undefined salmonid. [111] [112] Pearson sent almost all of the specimens collected to the Smithsonian, but the fossils were never accessioned into the collections and are now considered lost. He did retain one fossil from the initial collection which was later donated to the USGS collections. The largest single work on the fish of the Okanagan Highlands was published by Mark Wilson in 1977 and covered fossils collected from the known British Columbian Okanagan Highlands fossil sites of the time. [113] While not covering the Washington State fossils, Wilson named two of the species that are currently recognized from the Klondike Mountain Formation Amyzon aggregatum and Eosalmo driftwoodensis. Additionally scales attributed to the genus Amia were discussed and the genus Libotonius was named from fossils in the Allenby Formation. [114] [115] In the late 1960s a collection of fish from near the Tom Thumb Mine in Republic was compiled by resident R. Woodward. During the summers of 1976 and 1977 the University of Alberta conducted field collecting in both the Republic and Toroda Creek areas, along with the donation of the Woodward collection, yielded a number of fossil catostomids, along with a single percopsid, a salmonid, a hiodontid, and an Amia scale. The hiodontids were subsequently described as the species Eohiodon woodruffi in 1978 based on differences between the Tom thumb Tuff fossils and those found in British Columbian sites. [112] A year later the percopsid fossils were also described as Libotonius pearsoni, extending the range of the genus south from the Allenby Formation. [114]
Bird fossils are limited to mostly isolated feathers that are preserved in the finer grained strata of the lake bed, though one partial bird skeleton has also been recovered.
Family | Genus | Species | Authors | Year | Notes | Images |
---|---|---|---|---|---|---|
Wilson, 1977 | 1977 | A bowfin, known from isolated scales | ||||
† Amyzon | Wilson, 1977 | 1977 | A sucker | |||
† Amyzon | Unidentified [116] | (Wilson, 1977) | 1977 | A sucker, originally identified as Amyzon aggregatum | ||
† Eosalmo | Wilson, 1977 | 1999 | A Salmon | |||
Wilson, 1978 | 1978 | |||||
Wilson, 1979 | 1979 | A sand roller relative. | ||||
incertae sedis (Aves) | Unidentified | "Unnamed" [118] | 2019 | indeterminate feathers and a skeleton | ||
Tilia johnsoni is an extinct species of flowering plant in the family Malvaceae that, as a member of the genus Tilia, is related to modern lindens. The species is known from fossil leaves found in the early Eocene deposits of northern Washington state, United States and a similar aged formation in British Columbia, Canada.
Sassafras hesperia is an extinct species of flowering plant in the family Lauraceae.
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 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.
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.
Rhus malloryi is an extinct species of flowering plant in the sumac family Anacardiaceae. The species is known from fossil leaves found in the early Eocene deposits of northern Washington state, United States. The species was first described from a series of isolated fossil leaves in shale. R. malloryi is one of four sumac species to be described from the Klondike Mountain Formation, and forms a hybrid complex with the other three species.
The Coldwater Beds are a geologic formation of the Okanagan Highlands in British Columbia, Canada. They preserve fossils dating back to the Ypresian stage of the Eocene period, or Wasatchian in the NALMA classification.
Tsukada is an extinct genus of flowering plant in the family Nyssaceae related to the modern "dove-tree", Davidia involucrata, containing the single species Tsukada davidiifolia. The genus is known from fossil leaves found in the early Eocene deposits of northern Washington state, United States and a similar aged formation in British Columbia, Canada.
Comptonia columbiana is an extinct species of sweet fern in the flowering plant family Myricaceae. The species is known from fossil leaves found in the early Eocene deposits of central to southern British Columbia, Canada, plus northern Washington state, United States, and, tentatively, the late Eocene of Southern Idaho and Earliest Oligocene of Oregon, United States.
Carpinus perryae is an extinct species of hornbeam known from fossil fruits found in the Klondike Mountain Formation deposits of northern Washington state, dated to the early Eocene Ypresian stage. Based on described features, C. perryae is the oldest definite species in the genus Carpinus.
Klondikia is an extinct hymenopteran genus in the ant family Formicidae with a single described species Klondikia whiteae. The species is solely known from the Early Eocene sediments exposed in northeast Washington state, United States. The genus is currently not placed into any ant subfamily, being treated as incertae sedis.
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 1970s. The noted richness of agricultural plant families in Republic and Princeton floras resulted in the term "Eocene orchards" being used for the paleofloras.
Pteronepelys, sometimes known as the winged stranger, is an extinct genus of flowering plant of uncertain affinities, which contains the one species, Pteronepelys wehrii. It is known from isolated fossil seeds found in middle Eocene sediments exposed in north central Oregon and Ypresian-age fossils found in Washington, US.
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.
Alnus parvifolia was an extinct species of flowering plant in the family Betulaceae related to the modern birches. The species is known from fossil leaves and possible fruits found in early Eocene sites of northern Washington state, United States, and central British Columbia, Canada.
Republicopteron is an extinct orthopteran genus in the katydid-like family Palaeorehniidae with a single described species, Republicopteron douseae.
Republica is an extinct zygopteran genus in the damselfly family Euphaeidae with a single described species, Republica weatbrooki. The species is solely known from the Early Eocene sediments exposed in the northeast of the U.S. state of Washington.