Klondike Mountain Formation

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Klondike Mountain Formation
Stratigraphic range: Ypresian
50.1–48.9 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
Klondike Mountain Formation outcrop - Site A0307.JPG
Klondike Mountain Formation outcrop at site A0307
TypeGeological formation
Unit of
Sub-unitsTom Thumb Tuff, Lower & Upper Members
UnderliesGlacial deposits
Overlies & others
Thicknessup to 3,200 ft (980 m)
Lithology
PrimaryVariable
OtherSee text
Location
Coordinates48°42′N 118°42′W / 48.7°N 118.7°W / 48.7; -118.7Coordinates: 48°42′N 118°42′W / 48.7°N 118.7°W / 48.7; -118.7
Approximate paleocoordinates54°24′N 101°54′W / 54.4°N 101.9°W / 54.4; -101.9
RegionOkanagan highlands
Country United States
ExtentOkanagan highlands
Type section
Named for
Named byMuessig
Year defined1962
Klondike Mountain Formation is located in the United States
Klondike Mountain Formation
Klondike Mountain Formation (the United States)

The Klondike Mountain Formation is an Early Eocene (Ypresian) geological formation located in the northeast central area of Washington state. The formation, named for the type location designated in 1962, Klondike Mountain north of Republic, Washington, is composed of volcanic rocks in the upper unit and volcanics plus lacustrine (lakebed) sedimentation in which a lagerstätte with exceptionally well-preserved plant and insect fossils has been found, along with fossil epithermal hot springs.

The formation is the youngest in a group of formations which belong to the Challis Sequence rocks. The formation unconformably overlies rocks of the Eocene and much older Triassic and Permian formations. The formation is bounded on its edges by a series of high-angle strike slip faults, which have contained the Klondike Mountain Formation in a series of graben structures, such as the Republic Graben. Public access to a fossiliferous outcrop at the north end of Republic is mediated by the nonprofit Stonerose Interpretive Center.

Extent[]

The formation is located in northern Ferry County, Washington, with the majority of the sedimentation in the Republic and Curlew Basins on the east and in the Toroda Creek area to the north west. The town of Republic, Washington is situated at the southern end of the formation, with outcrops within the city itself. The formation was named for Klondike Mountain which is just to the northeast of the city, and where the type locality is located.[1] The Curlew basin is situated north of Republic, with the northern edge along the Kettle River and the community of Curlew, Washington near the northeastern edge.[2][3]

The formation is the southernmost of a string of preserved Eocene highland lakebeds in Washington state and British Columbia.[4] The lake system, within the Okanagan highlands, extends from the Klondike Mountain Formation north approximately 1,000 kilometres (1,000,000 m) in to southern central British Columbia.[5]

Age[]

Early dating of the formation was based primarily on identification and correlation of the fossils found in the Tom Thumb Tuff, with Joseph Umpleby (1910) reporting a putative age of Early Miocene.[6] This date was based in examination of fossils by C. R. Eastman, who thought them to be similar to those found in the Florissant Formation of Colorado, which at the time was also considered Miocene. This age was retained by Edward W. Berry (1929), who included the Klondike Mountain Formation fossil lakebeds as part of the Latah Formation.[7] The age of the Formation has been revised in the following hundred years, with Roland W. Brown (1936) identifying the deposits as being older than the Latah Formation.[8] In a later written communication circa 1958, Brown again revised the age still older, stating the fossils found in the area of Mount Elizabeth indicated an Oligocene age. This age was used by Parker and Calkins (1964) for work on the Curlew Quadrangle of Ferry County.[9] Work by Pearson and Obradovich (1977) refined the Sanpoil Volcanics age to between 52 to 51 million years ago, and a general age estimate for the Klondike Mountain Formation between 50.3 ± 1.7 million years ago and 42.3 ± 2.0 million years ago.[10] Since then the fossil-bearing strata of the Formation have been radiometrically dated, to give an estimate of the Ypresian, the mid stage of the early Eocene,49.4 ± .5 million years ago,[5] which was revised to an oldest age estimate of 51.2 ± 0.1 million years ago which given based on detrital zircon isotopic data published in 2021.[11]

Lithology[]

Parker and Calkins (1964) noted the association of the Klondike Mountain Formation with the gold and silver deposits of the Republic District and suggested it as a potential host to more ore deposits in the Curlew Quadrangle.[9] The epithermal gold deposits occurring in the Sanpoil volcanics terminate directly below the unconformity where the volcanics contact the base of the Klondike Mountain Formation[12] or sometimes penetrate into the Formation's lowest unit.[13] Hydrothermal sinter deposits are known from the lowest portions of the Formation and are thought to represent hydrothermal eruption areas.[13] In general the lower portions of the Formation have a large amount of hydrothermal alteration, and areas around vents are rich in pyrite and silica. two products of natural hydrothermic sintering. The areas above that show a transition to mudstones, siltstones and sandstones grading from fine-grained material into coarser materials moving up the strata column. The finely-bedded stones show the greatest numbers of fossils and the finest preservation of details.[14]

Paleoenvironment and paleoclimate[]

The lake bed sediments preserve a diverse array of plants, insects, and fishes, notably the biota called the Republic flora.[15] The Okanagan lake system, which includes the Klondike Mountain Formation, has been classified as one of the great Canadian lagerstätten.[16] The area likely had a mesic upper microthermal to lower mesothermal climate, in which winter temperatures rarely dropped low enough for snow, and which were seasonably equitable.[17]

The Okanagan highlands paleoforest surrounding the lakes have been described as precursors the to modern Temperate broadleaf and mixed forests of Eastern North America and Eastern Asia. Based on the fossil biotas the lakes were higher and cooler then the coeval coastal forests preserved in the Puget Group and Chuckanut Formation of Western Washington, which are described as lowland tropical forest ecosystems. Estimates of the paleoelevation between 0.7–1.2 km (0.43–0.75 mi) higher than the coastal forests. This is consistent with the paleoelevation estimates for the lake systems, which range between 1.1–2.9 km (1,100–2,900 m), which is similar to the modern elevation 0.8 km (0.50 mi), but higher.[17]

Estimates of the mean annual temperature have been derived from Climate leaf analysis multivariate program (CLAMP) and leaf margin analysis (LMA) of the Republic paleoflora. The CLAMP results after multiple linear regressions for Republic gave a mean annual temperature of approximately 8.0 °C (46.4 °F), while the LMA gave 9.2 ± 2.0 °C (48.6 ± 3.6 °F). This is lower than the mean annual temperature estimates given for the coastal Puget Group, which is estimated to have been between 15–18.6 °C (59.0–65.5 °F). The bioclimactic analysis for Republic suggests a mean annual precipitation amount of 115 ± 39 cm (45 ± 15 in).[17]

Paleobiota[]

The formation is host to a highly diverse assemblage of plants and insects including some of the last records of taxa before extinction and the first appearances of taxa.

Lycophytes[]

Family Genus Species Authors Year Notes Images

Selaginellaceae

Selaginella

Undescribed[18]

A spikemoss
Not described to species

Pteridophytes[]

Family Genus Species Authors Notes Images

Cystopteridaceae

Cf. Cystopteris

Undescribed[18]

A possible bladder fern relative
Not described to species

Equisetaceae

Equisetum

Undescribed[19][18]

A scouring rush
Not described to species

Lygodiaceae

Lygodium

Undescribed[18][17]

A climbing fern
Not described to species

Salviniaceae

Azolla

Azolla primaeva[20]

Arnold

A mosquito fern

Azolla primaeva

Salviniaceae

Salvinia

Undescribed[21]

A "watermoss" species.
Not described to species
Found only in Curlew half graben sites.

Gymnosperms[]

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 pf Ginkgo, while an undescribed Zamiaceae member is the sole cycadophyte.

Cycadophytes[]

Family Genus Species Authors Notes Images

Zamiaceae

Undescribed

Undescribed[22][23]

A zamiaceous cycad.
Not described to genus/species

Undescribed zamiaceous leaf

Gingkophytes[]

Family Genus Species Authors Notes Images

Ginkgoaceae

Ginkgo

Ginkgo biloba[24]

Linnaeus

A ginkgo

Ginkgo biloba

Ginkgoaceae

Ginkgo

Ginkgo dissecta[24]

A ginkgo

Ginkgo dissecta

Pinophytes[]

Family Genus Species Authors Notes Images

Cupressaceae

Calocedrus

Undescribed[23][25]

An incense cedar
Not described to species

Cupressaceae

Chamaecyparis

Undescribed[26]

A false cypress
Not described to species
Possibly in the Callitropsis nootkatensis lineage.[27]

Cupressaceae

Cryptomeria

Undescribed[26][17]

A sugi
Not described to species

Cupressaceae

Glyptostrobus

Undescribed[26]

A Chinese swamp cypress
Not described to species

Cupressaceae

Metasequoia

Metasequoia occidentalis[28][15]

(Newberry) Chaney

A dawn redwood

Cupressaceae

Sequoia

Sequoia affinis[28]

Lesquereux

A coast redwood
Reported as "Sequioa langsdorfii" by Brown, 1935

Cupressaceae

Taiwania

Undescribed[21]

A Taiwania species
not described to species

Cupressaceae

Taxodium

Taxodium dubium[7][28]

(Sternberg) Heer

A bald cypress

Cupressaceae

Thuja

Undescribed[26]

An arborvitae
Not described to species

Pinaceae

Abies

Abies milleri[29]

& Wehr

Oldest true fir described

Pinaceae

Picea

Undescribed[26]

A spruce
Not described to species

Pinaceae

Pinus

Pinus latahensis[7]

Berry

A 5 needle pine

Pinaceae

Pinus

[7]

Berry

A 3 needle pine, jr homonym to Pinus macrophylla Lindley 1839

Pinaceae

Pinus

[7]

Berry

A pine seed morphogenus

Pinaceae

Pinus

[7]

Berry

A possible 4 needled pine
Noted by Berry as
"highly improbable that this should represent a distinct botanic species"

Pinaceae

Pseudolarix

Pseudolarix wehrii[30]

Gooch

A golden larch
Originally described as Pseudolarix americana.[30]

Pinaceae

Tsuga

Undescribed[26]

A hemlock
Not described to species

Sciadopitys

Undescribed[26]

An umbrella pine
Not described to species

Sciadopitys species

Taxaceae

Amentotaxus

Undescribed[26]

A yew
Not described to species

Taxaceae

Cephalotaxus

Undescribed[26]

A yew
Originally described placed in the Miocene [7][31]
Not described to species

Taxaceae

Taxus

Undescribed[26]

A yew
Not described

Flowering plants[]

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.[32] 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.

Nymphaeales[]

The Basal Angiosperms are represented by a single Nymphaeales water-lily species Nuphar carlquistii.,[33] though a second member, , has been described from the Princeton Chert.[34] Wehr (1995) illustrated two fossils that were tentatively identified as fruits of the banana genus Ensete and the extinct myrtle genus respectively,[35] 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.[33]

Family Genus Species Authors Notes Images

Nymphaeaceae

Nuphar

Nuphar carlquistii[33]

DeVore, Taylor, & Pigg

A waterlily,
Rhizome sections were first identified as Ensete
Seed masses first identified as .

Nuphar carlquistii seeds

Magnoliids[]

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 has described from permineralized wood in the Princeton Chert.[36] 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 representing the oldest confident Saururaceae species in the fossil record.[37]

Family Genus Species Authors Notes Images

Lauraceae

Undescribed[18]

A lauraceous form species.
Not described to species

Lauraceae

Ocotea

Undescribed[18]

A stinkwood species.
Not described to species

Lauraceae

Phoebe

Undescribed[15]

A Phoebe species.
Not described to species

Lauraceae

Sassafras

Sassafras hesperia[15]

Berry

A sassafras

Magnoliaceae

Magnolia

Undescribed[38]

A magnolia, possibly Magnolia subgenus Talauma
Not described to species

incertae sedis

Dillhoffia

Dillhoffia cachensis[39]

Manchester & Pigg

A flower of uncertian floral affinity

Dillhoffia cachensis

Monocots[]

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 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 ,[40] the alismatalean genus ,[41] the alismatalean ,[42] the asparagalean pollen morphogenus ,[43] the lilialean genus ,[44] and the poalean genus ,[45]

Family Genus Species Authors Notes Images

Amaryllidaceae

[46]

Pigg, , & DeVore

An onion relative

Araceae

Orontium

Orontium wolfei[47]

Bogner, Johnson, & Upchurch

A golden club

Orontium wolfei

Smilacaceae

Smilax

Undescribed[18]

A greenbrier species.
Not described to species.

Typhaceae

Typha

Undescribed[18]

A cattail species.
Not described to species.

Eudicots[]

Rhus hybrid leaf with lobed terminal leaflet

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.[48] Benedict et al. (2011) described first fossils for the prunoid genus Oemleria along with the oldest Prunus flowers. The Prunus flowers are complimented by leaf fossils representeding five to six distinct morphotypes.[49] Spiraea is known from an 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 leaves belonging to either Malus or Pyrus have been found. Two distinct species of the Asian endemic genus Photinia are known, however only on of them had been described as of 2007.[49] The rosaceous genus Physocarpus had been reported by Hopkins and Wehr (1994) as also occurring in the formation,[38] 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.[50]

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.[51] 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.[52] If fossils of the fruits and foliage in attachment are found, that would bring the species count down to three whole plant taxa.[52] Additionally, the extinct genus 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.[53] Wesley Wehr in 1994 reported Bignoniaceae seeds along with a single Rubiaceae fruit and an isolated Fabaceae leaf.[54] 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.[35]

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.[55] That status was affirmed by Forest et al. (2005) who used both as fossil calibration points for phylogenetic analysis of Betulaceae.[56]

Family Genus Species Authors Notes Images

Anacardiaceae

Rhus

Rhus boothillensis[51]

Flynn, DeVore, & Pigg

A sumac,
Hybridized with other Klondike Mountain Formation Rhus

Anacardiaceae

Rhus

Rhus garwellii[51]

Flynn, DeVore, & Pigg

A sumac,
Hybridized with other Klondike Mountain Formation Rhus

Anacardiaceae

Rhus

Rhus malloryi[15][51]

(Wolfe and Wehr) Flynn, DeVore & Pigg

A sumac,
Hybridized with other Klondike Mountain Formation Rhus

Anacardiaceae

Rhus

Rhus republicensis[51]

Flynn, DeVore, & Pigg

A sumac,
Hybridized with other Klondike Mountain Formation Rhus

Aquifoliaceae

Ilex

Undescribed[17]

A holly
Not described to species

Araliaceae

Aralia

Undescribed[23]

A spikenard species
Not described to species.

Betulaceae

Alnus

[15]

(Berry) Wolfe & Wehr

An Alder

Betulaceae

Betula

Betula leopoldae[15][57]

Wolfe & Wehr

A birch

Betula leopoldae

Betulaceae

Carpinus

Carpinus perryae[55]

Pigg, , & Wehr

A hornbeam

Betulaceae

Corylus

Corylus johnsonii[55]

Pigg, , & Wehr

A hazel nut

Betulaceae

[55]

Pigg, Manchester, & Wehr

A birch relative

Betulaceae

Undescribed[55]

A birch relative
different from the other Okanagan Highlands species

undescribed species

Bignoniaceae

Undescribed

Undescribed[54]

A catalpa family member
Not described to species

Bignoniaceae sp. fruit

Burseraceae

Barghoornia

Barghoornia oblongifolia[15]

Wolfe & Wehr

An extinct Bursera relative

Barghoornia oblongifolia

Celtidaceae

Pteroceltis

Undescribed[58]

A cannabaceous fruit
Not described to species

Pteroceltis species fruit

Cercidiphyllaceae

Cercidiphyllum

[15]

(Dawson) Wolfe & Wehr

A katsura with suggested affinity to †,[23]
First described as "Populus" obtrita

Cornaceae

Cornus

Undescribed[15][23][17]

A dogwood species,
Not described to species

Elaeocarpaceae

Sloanea

Undescribed[58]

An elaeocarpaceous fruit
Not described to species

Ericaceae

Arbutus

Undescribed[38][17]

A madrone relative
Not described to species

Ericaceae

Rhododendron

Undescribed[38][23][17]

A rhododendron
Not described to species

Ericaceae

Cf. Leucothoe

Undescribed[38]

A doghobble relative
Not described to species

Eucommiaceae

Eucommia

Eucommia montana[59][17]

Brown

A "hard rubber tree"

Eucommia montana

Fagaceae

Undescribed[17]

A Castanea relative
Not described to species

Fagaceae

[15]

(Knowlton) Hollick

A beech relative

Fagaceae

Fagus

[60]

Manchester & Dillhoff

A beech

Fagaceae

Quercus

Undescribed[54][23][17]

An oak
Not described to species

Grossulariaceae

Ribes

"Species 1"[38][23][17]

A current
Not described to species

Grossulariaceae

Ribes

"Species2"[38]

A current
Not described to species

Hamamelidaceae

Corylopsis

Corylopsis reedae[38][61]

, , & Wehr

A winter-hazel

Corylopsis reedae

Hamamelidaceae

Fothergilla

Fothergilla malloryi[61]

Radtke, Pigg, & Wehr

A witch alder

Fothergilla malloryi

Hamamelidaceae

Langeria

Langeria magnifica[15]

Wolfe & Wehr

A witch hazel relative

Langeria magnifica

Hydrangeaceae

Hydrangea

Undescribed[38]

A Hydrangea.
Not described to species

Hydrangeaceae

Philadelphus

Undescribed[38]

A mock-orange
Not described to species

Icacinaceae

Unidentified[54][23]

A Phytocrene relative
Not described to species

Iteaceae

Itea

Undescribed[15][17]

A virginia willow species
Not described to species.

Juglandaceae

Carya

Undescribed[23][17]

A walnut family relative.
Not described to species.

Juglandaceae

[62]

(Brown) Manchester

A walnut family relative.

Juglandaceae

Juglans

Undescribed[23][17]

A walnut family relative.
Not described to species.

Juglandaceae

Pterocarya

Undescribed[54]

A wing nut
Not described to species

Lythraceae

Decodon

Undescribed[23]

A swamp loosestrife
Not described to species

Malvaceae

Craigia

Undescribed[54]

A Craigia species
Not described to species

Malvaceae

Florissantia

Florissantia quilchenensis[63]

( & ) Manchester

A chocolate relative

Florissantia quilchenensis

Malvaceae

Hibiscus

Undescribed[38]

A hibiscus
Not described to species

Malvaceae

Undescribed[54]

A relative
Not described to species

Malvaceae

Tilia

Tilia johnsoni[15]

Wolfe & Wehr

A Linden

Tilia johnsoni

Malvaceae

Cf. Tilia

Undescribed[58]

Linden relative fruits
Not described to species

Cf. Tilia fruits

Menispermaceae

Calycocarpum

Undescribed[35]

A moonseed
Not described to species

Moraceae

Morus

Undescribed[38]

A mulberry, two types known.
Not described to species

Myricaceae

Comptonia

Comptonia columbiana[15]

Dawson

A Comptonia

Nyssaceae

Tsukada

Tsukada davidiifolia[15]

Wolfe & Wehr

A dove-tree relative

Tsukada davidiifolia

Platanaceae

Undescribed[54]

Manchester

A plane tree fruit taxon
Not described to species

species

Platanaceae

Macginitiea

Macginitiea gracilis[15]

(Lesquereux) Wolfe & Wehr

A plane tree relative

Macginitiea gracilis

Platanaceae

Undescribed[58]

A sycamore stamen head
isolated stamen clusters placed as
Not described to species

stamen cluster

Polygalaceae

Undescribed[54]

A milkwort relative
Not described to species

Ranunculaceae

Clematis

Undescribed[38]

A Clematis
Not described to species

Clematis species

Rosaceae

Amelanchier

Undescribed[38]

A service berry
Not described to species

Rosaceae

Malus

Undescribed[17]

An apple
Not described to species

Rosaceae

Neviusia

Undescribed[38]

A snow-wreath
Not described to species

Rosaceae

Oemleria

[48]

, DeVore, & Pigg

An Osoberry

Rosaceae

Photinia

[15]

Wolfe & Wehr

A Christmas-berry relative

Rosaceae

Prunus

[48]

Benedict, DeVore, & Pigg

A cherry relative

Rosaceae

Prunus

"Species 1"[15]

A prunoid leaf
Not described to species

Rosaceae

Prunus

"Species 2"[15]

A prunoid leaf
Not described to species

Rosaceae

Prunus

"Species 3"[15]

A prunoid leaf
Not described to species

Rosaceae

Pyracantha

Undescribed[49]

A firethorn sp.[49]
Tentative record, Not described to species.

Rosaceae

Rubus

Undescribed[38]

A blackberry
Not described to species

Rosaceae

Spiraea

Undescribed[23][17]

A bridal wreath
Not described to species.

Rosaceae

Aff. Sorbus

Undescribed[23][17]

A rowan relative
Not described to species.

Rosaceae

Aff. Physocarpus

Undescribed[23]

A possible nine-bark
Not described to species
Possibly stem Neillieae[50]

Rosaceae

Cf. Crataegus

Undescribed[38]

A hawthorn relative
Not described to species

Rosaceae

Cf. Malus

Undescribed[49]

A maloid species possibly apple or pear
Not described to species

Rosaceae

Cf. Spiraea

Undescribed[49]

A bridal wreath relative
Not described to species

Rosaceae

Cf. Pyrus

Undescribed[49]

A maloid species possibly apple or pear
Not described to species

Sabiaceae

Meliosma

Undescribed[35]

A Meliosma species
Not described to species

Sabiaceae

Undescribed[35]

A species
Not described to species

Salicaceae

Populus

Undescribed[23][17]

A cottonwood
Not described to species
First identified as †[7]

Salicaceae

Undescribed[23]

A
Not described to species

Salicaceae

Salix

Undescribed[23][17]

A willow
Not described to species

Sapindaceae

Acer?

[64]

Heer, 1876

A possible maple

Sapindaceae

Acer

Acer hillsi[64]

Wolfe &

A maple

Sapindaceae

Acer

Acer republicense[64]

Wolfe & Tanai

A maple

Sapindaceae

Acer

Acer spitzi[64]

Wolfe & Tanai

A maple

Sapindaceae

Acer

Acer stonebergae[64]

Wolfe & Tanai

A maple

Sapindaceae

Acer

Acer toradense[64]

Wolfe & Tanai

A maple

Sapindaceae

Acer

Acer washingtonense[64]

Wolfe & Tanai

A maple

Sapindaceae

Acer

[64]

Wolfe & Tanai

A maple

Sapindaceae

Aesculus

Undescribed[23][65]

A horse chestnut
Not described to species.

Sapindaceae

[15]

(Brown) Wolf & Wehr

An extinct sapindalean species

Sapindaceae

Dipteronia

Dipteronia brownii[66]

&

A Dipteronia

Sapindaceae

Koelreuteria

[67]

Wang et al.

A Koelreuteria species

Sapindaceae

Cf. Boniodendron

[15][67]

Becker

A sapindaceous species
first described as a Koelreuteria species,
considered Cf. Boniodendron by Wang et al (2012).

Schisandraceae

Kadsura

Undescribed[18]

A kadsura species.
Not described to species

Schoepfiaceae

Schoepfia

[15]

(LaMotte) Wolfe & Wehr

A possible Schoepfia relative,
First described as "Cornus acuminata.

Theaceae

"Species A"[15]

A theaceous species similar to Gordonia
Not described to species

Theaceae

"Species B"[15]

A theaceous species similar to Cleyera
Not described to species

Trochodendraceae?

Undescribed[54]

A trochodendroid of uncertain placement.[53]
Fruits of the leaf taxon
Not described to species.

Trochodendraceae

Paraconcavistylon

Paraconcavistylon wehrii[52][53]

( et al.)

A Trochodendrale
first described as "Concavistylon" wehrii
moved to a new genus in 2020.

Trochodendraceae

Pentacentron

Pentacentron sternhartae[52]

et al.

A Trochodendrale

Pentacentron sternhartae

Trochodendraceae

Tetracentron

Tetracentron hopkinsii[52]

Pigg et al.

A Trochodendrale,
possibly the leaves of Pentacentron sternhartae

Trochodendraceae

Trochodendron

Trochodendron nastae[68]

Pigg, Wehr, &

A Trochodendron
Possibly the leaves of Trochodendron drachukii

Trochodendraceae

Undescribed[23]

A trochodendroid of uncertain placement.[53]
Leaves of the fruit taxon
Not described to species.

Ulmaceae

Undescribed[35]

An elm relative
Not described to species

Ulmaceae

Ulmus

[69]

(Berry) LaMotte

An elm species

Ulmaceae

Ulmus

Ulmus okanaganensis

Denk & Dillhoff

An elm species,
the fruits were first identified as Ulmus section Chaetoptelea.

Ulmus okanaganensis

Vitaceae

Vitis

Undesribed[38][54]

Grape seeds[54] and leaves[38]
Not described to species

Incertae sedis

Undescribed[23]

A leaf morphotype of uncertain affiliation.
Not described to species.

incertae sedis

[54]

Crane

A winged fruit of unidentified affinities

incertae sedis

Pteronepelys

Pteronepelys wehrii[70]

Manchester

A samara of uncertain affinities.

Pteronepelys wehrii

incertae sedis

[15]

Wolfe & Wehr

An incertae sedis angiosperm
possibly of Hamamelididae affiliations

Arthropods[]

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.[71] The most prevalent orders are Diptera and Hemiptera, each making up approximately 30% of the fossil insects known in 1992.

Blattodea[]

Family Genus species Authors Notes Images

Blaberidae

Undescribed

Undescribed[17]

A cockroach
Not described to genus/species

Blattoidae

Undescribed

Undescribed[71]

A blattoidean cockroach
Not described to genus/species

Undescribed Blattoidea

Isoptera

Undescribed

Undescribed[71]

Undescribed termites of uncertain affiliation

undescribed isopteran

Coleoptera[]

A list of Coleopteran families identified by 1992 included Carabidae, Cerambycidae, Chrysomelidae, Curculionidae, Dytiscidae, Elateridae and Lucanidae,[71] but the beetle fauna has not been described in depth yet, with only two weevil species having been fully described.[72][73] A third beetle group belonging to the bean beetle tribe has been identified as palm beetles of the genus group.[74]

Family Genus Species Authors Notes Images

Brentidae

[72]

Legalov, 2013

An Ithycerinae weevil

Brentidae

[73]

Legalov, 2015

An Ithycerinae weevil

Carabidae

Undescribed

Undescribed[71]

A ground beetle
Not described to genus/species

Unidentified Carabidae

Cerambycidae

Undescribed

Undescribed[71]

A long-horn beetle
Not described to genus/species

Chrysomelidae

genus group

Undescribed[74]

palm beetles in the tribe .
Not described to genus/species

Dytiscidae

Undescribed

Undescribed[71]

A diving beetle
Not described to genus/species

Elateridae

Undescribed

Undescribed[71]

A click beetle
Not described to genus/species

Lucanidae

Undescribed

Undescribed[71]

A stag beetle
Not described to genus/species

Dermaptera[]

The order Dermaptera was first reported in 1992[71] 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.[75]

Family Genus Species Authors Notes Images

Forficulidae?

Unidentified

"Forficulid species 1"[75]

A possible forficulid earwig with long cerci
Not described to genus/species

"Forficulid species 1"

Forficulidae?

Unidentified

"Forficulid species 2"[75]

A possible forficulid earwig with short cerci
Not described to genus/species

Diptera[]

Family Genus Species Authors Notes Images

Bibionidae

Undescribed

Undescribed[71]

A march fly
Not described to genus/species

unidentified Bibionidae

Mycetophilidae

Undescribed

Undescribed[71]

A fungus gnat
Not described to genus/species

Pipunculidae

Metanephrocerus

Metanephrocerus belgardeae[76]

Archibald, , & Mathewes, 2014

A pipunculid big-headed fly

Metanephrocerus belgardeae

Tipulidae

Undescribed

Undescribed[71]

A crane fly
Not described to genus/species

Undescribed Tipulidae

Ephemeroptera[]

Lewis (1992) listed one species of Heptageniidae mayflies and three specimens that he did not place to family.[71] The Heptageniidae specimen was later described as a squaregill mayfly by Sinitchenkova (1999) and the oldest member of the genus Neoephemera.[77]

Family Genus Species Authors Notes Images

Neoephemeridae

Neoephemera

Neoephemera antiqua[77]

, 1999

A squaregill mayfly,
first tentatively identified as a flat headed mayfly.[71]

Hemiptera[]

Family Genus Species Authors Notes Images

Aphididae

Undescribed

Undescribed[71]

An aphid
Not described to genus/species.

Aphrophoridae

Aphrophora

Undescribed[71]

An aphrophorid spittlebug
Not described to species.

Aphrophora species

Aphrophoridae

Undescribed[71]

An aphrophorid spittlebug
Not described to species.

Cercopidae

Undescribed[71]

A cercopid froghopper
Not described to species.

Cercopidae

Undescribed

Undescribed[71]

A cercopid froghopper
Not described to genus/species.

undescribed Cercopidae

Fulgoroidea

Undescribed

Undescribed[71]

A frog hopper
Not described to genus/species.

Pentatomidae

Undescribed

Undescribed[71]

A Shield or stink bug
Not described to genus/species

undescribed Pentatomidae

Hymenoptera[]

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.[78]

Family Genus Species Authors Notes Images

Angarosphecidae

Undescribed[78]

An angarosphecid spheciform wasp.
Not described to species

Angarosphecidae

Undescribed

Undescribed[78]

An angarosphecid spheciform wasp
Likely not .
Not described to species

Braconidae

Undescribed

Undescribed[71][78]

braconid parasitic wasps
Not described to genus/species.

Unidentified Braconidae

Cimbicidae

Undescribed

Undescribed[78]

A cimbicid sawfly.
Not Described to genus/species

Unidentified Cimbicidae

Diapriidae

Undescribed

Undescribed[78]

A diapriid diaprioid wasp
Not described to species

Formicidae

Klondikia

Klondikia whiteae[79]

Dlussky & Rasnitsyn, 2003

An ant of uncertain subfamily affiliation

Formicidae

Myrmeciites

"Indesterminate"[80]

Archibald, , & , 2006

A bulldog ant form genus

sp.

Formicidae

Oecophylla

[81]

(Dlussky & Rasnitsyn, 1999)

An ant, described as Camponotites kraussei,
Moved to Oecophylla kraussei in 2017[82]

Formicidae

Propalosoma

Propalosoma gutierrezae[81]

Dlussky & Rasnitsyn, 1999

A bulldog ant, first described as a Rhopalosomatidae wasp,
moved to myrmeciinae in 2018[83]

Propalosoma gutierrezae

Formicidae

Undescribed

Undescribed[78]

Ants of uncertain subfamily placement.[78]

Unidentified formicidae

Halictidae (?)

Undescribed

Undescribed[78]

A possible sweat bee
Not described to genus/species

Ichneumonidae

Undescribed

Undescribed[78]

ichneumonid parasitic wasps unplaced to subfamily
Not described to genus/species

Undescribed Ichneumonidae

Megachilidae

Undescribed

Undescribed[78]

Megachilid leaf-cutter bee herbivory trace fossils on leaves
Not described to genus/species

Pamphiliidae

Ulteramus

Ulteramus republicensis[84]

Archibald & Rasnitsyn, 2015

A parasitic wasp

Pompilidae

Undescribed

Undescribed[78]

A pompilid spider wasp
Not described to genus/species

Proctotrupidae

Undescribed

Undescribed[78]

A proctotrupid parasitic wasp
Not described to genus/species

Roproniidae

Undescribed

Undescribed[78]

A roproniid (sensu lato) proctotrupoid wasp
Not described to genus/species

Scoliidae

Undescribed

Undescribed[78]

An scoliid wasps
Not described to genus/species

Sphecidae

Undescribed

Undescribed[78]

A sphecid (sensu stricto) wasp
Not described to genus/species

Tenthredinidae

Undescribed

Undescribed[78]

A Tenthredinid sawfly
Not described to genus/species

Vespidae

Undescribed

Undescribed[78]

A vespid wasp
Not described to genus/species

Lepidoptera[]

A solitary lepidopteran 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]

Family Genus Species Authors Year Notes Images

Erebidae

Undescribed

Undescribed[85]

1986

An arctiine tiger moth
Not described

Mecoptera[]

A number of mecopteran species belonging to the families Cimbrophlebiidae, Dinopanorpidae, Eorpidae, and Panorpidae are also known.[86]

Family Genus Species Authors Year Notes Images

Cimbrophlebiidae

Cimbrophlebia

[86]

Archibald, 2009

2009

A Cimbrophlebiid scorpionfly

Cimbrophlebiidae

Cimbrophlebia

[86]

Archibald, 2009

2009

A Cimbrophlebiid scorpionfly

Dinopanorpidae

Dinokanaga

Dinokanaga andersoni[87]

Archibald, 2005

2005

A scorpion fly species

Dinokanaga andersoni

Dinopanorpidae

Dinokanaga

Dinokanaga dowsonae[87]

Archibald, 2005

2005

A scorpion fly species

Dinopanorpidae

Dinokanaga

Dinokanaga sternbergi[87]

Archibald, 2005

2005

A scorpion fly species

Eorpidae

Eorpa

Eorpa elverumi[88]

Archibald, Mathewes, & Greenwood, 2013

2013

A mecopteran scorpionfly

Eorpa elverumi

Eorpidae

Eorpa

?†Eorpa ypsipeda[88]

Archibald, Mathewes, & Greenwood, 2013

2013

A mecopteran scorpionfly, tentatively identified

Possible E. ypsipeda[88]

Neuroptera[]

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.[5]

Family Genus Species Authors Year Notes Images

Chrysopidae

[89]

& , 2013

2013

A green lacewing

Hemerobiidae

Proneuronema

Proneuronema wehri[90][91]

(Makarkin, Archibald, & , 2003)

2003

A hemerobiid lacewing, originally placed in †Cretomerobius,
moved to †Proneuronema in

Ithonidae

Allorapisma

Allorapisma chuorum[92]

Makarkin & Archibald, 2009

2009

A moth lacewing

Allorapisma chuorum

Ithonidae

Palaeopsychops

Palaeopsychops marringerae[93]

Archibald & Makarkin, 2006

2006

A polystechotid group[94] moth lacewing

Palaeopsychops marringerae

Ithonidae

Palaeopsychops

Palaeopsychops timmi[93]

Archibald & Makarkin, 2006

2006

A polystechotid group[94] moth lacewing

Palaeopsychops timmi

Ithonidae

[93]

Archibald & Makarkin, 2006

2006

A polystechotid group[94] moth lacewing

Ithonidae

[93]

Archibald & Makarkin, 2006

2006

A polystechotid group[94] moth lacewing

Ithonidae

[93]

Archibald & Makarkin, 2006

2006

A polystechotid group[94] moth lacewing

Nymphidae

?Nymphes

Nymphes? georgei[95]

Archibald, Makarkin, & Ansorge, 2009

2009

A nymphid lacewing, possibly a species of †[96]

Osmylidae

[97]

Makarkin, Archibald, & Mathewes, 2021

2021

A osmylid lacewing

Psychopsidae?

Ainigmapsychops

Ainigmapsychops inexspectatus[5]

Makarkin & Archibald, 2014

2014

A possible psychopsid lacewing

Ainigmapsychops inexspectatus

Odonata[]

Family Genus Species Authors Year Notes Images

Aeshnidae

[98]

Archibald & Cannings, 2019

2019

A darner dragonfly

Aeshnidae

[98]

Archibald & Cannings, 2019

2019

A darner dragonfly

Aeshnidae

[98]

Archibald & Cannings, 2019

2019

A darner dragonfly

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

[99]

Archibald & Cannings, 2021

2021

A odonate

Euphaeidae

[100]

Archibald & Cannings, 2021

2021

A gossamerwing damselfly.
Not to be confused with the plant ,
also from the formation

[99]

Archibald & Cannings

2021

A possibly odonate

Phasmatodea[]

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.[101] 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.[102]

Family Genus Species Authors Year Notes Images

Susumaniidae

Eoprephasma

Eoprephasma hichensi[101]

Archibald & Bradler, 2015

2015

A Susumaniinae stick insect species

Raphidioptera[]

Family Genus Species Authors Year Notes Images

Raphidiidae

[103]

Archibald & Makarkin, 2021

2021

A raphidiid snakefly

Vertebrates[]

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.[104] 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, , 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.[105] Research tapered off until a series of fish were collected in the Toroda Creek Graben northwest of Republic by R. C. Pearson during his compilation of the Geologic map of the quadrangle, Ferry and Okanogan Counties, Washington. The fossils were tentatively identified by paleoichthyologist David Dunkle as members of the genera Amyzon, , and an undefined salmonid.[106] Pearson sent almost all of the specimens collected to the Smithsonian, but the fossils were never accessioned into the collections there 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.[107] 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.[108][109] 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.[106] A year later the percopsid fossils were also described as Libotonius pearsoni, extending the range of the genus south from the Allenby Formation.[108]

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

Amiidae

Amia

"Amia" hesperia

, 1977

1977

A bowfin, known from isolated scales

"Amia" hesperia scale

Catostomidae

Amyzon

Amyzon aggregatum

Wilson, 1977

1977

A sucker

Catostomidae

Amyzon

Unidentified[110]

(Wilson, 1977)

1977

A sucker, originally identified as Amyzon aggregatum

Salmonidae

Eosalmo

Eosalmo driftwoodensis[111]

Wilson, 1977

1999

A Salmon

Eosalmo driftwoodensis

Hiodontidae

Hiodon

Hiodon woodruffi[106]

Wilson, 1978

1978

A mooneye, first described as "Eohiodon" woodruffi.[106]

Libotoniidae

Libotonius

Libotonius pearsoni[108]

Wilson, 1979

1979

A sand roller relative.

Libotonius pearsoni

incertae sedis (Aves)

Unidentified

"Unnamed"[112]

2019

indeterminate feathers and a skeleton

Unidentified feather

References[]

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  3. ^ Cheney, ES; Rasmussen, MG (1996). "Regional geology of the Republic area". Washington Geology. 24 (2): 3–7.
  4. ^ Suydam, J.; Gaylord, D.R. (1997). "Toroda Creek half graben, northeast Washington: Late-stage sedimentary infilling of a synextensional basin". Geological Society of America Bulletin. 109 (10): 1333–1348. Bibcode:1997GSAB..109.1333S. doi:10.1130/0016-7606(1997)109<1333:tchgnw>2.3.co;2.
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