Allenby Formation
{{Short description|Sedimentary rock formation in British Columbia, Canada}}
{{for|Allenby Coal member|Carbondale Formation}}
{{Infobox rockunit
| name = Allenby Formation
| period = Ypresian
| age = Ypresian
{{fossilrange|52.5|48}}
| image = File:Princeton Chert sequence .jpg
| caption = Alternating Princeton Chert and coal sequences
| type = Geological formation
| prilithology = Shale, sandstone
| otherlithology = Coal–breccia, coal–chert
| namedfor = Allenby, British Columbia
| namedby = Shaw
| year_ts = 1952
| region = British Columbia
| country = Canada
| coordinates = {{Coord|49|22.6|N|120|32.8|W|display=title,inline}}
| paleocoordinates = {{coord|53.1|N|107.5|W|display=inline}}
| unitof = Princeton Group, Eocene Okanagan Highlands
| subunits = Princeton Chert, Vermillion Bluffs Shale
| underlies =
| overlies = Cedar Formation
| thickness = {{convert|1860|-|2100|m|ft|abbr=on}}
| extent = Princeton Basin & Tulameen basin
| area = {{convert|300|km2|sqmi|abbr=on}}
| map = {{Location map+ | Canada#British Columbia
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | Canada#British Columbia
| lat_deg = 49.4
| lon_deg = -120.5
| mark = Orange pog.svg
| marksize = 10
}}
}}
| map_caption =
}}
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.
{{TOC limit|3}}
Extent and correlation
The Allenby is estimated to have an overall extent of approximately {{convert|300|km²|sqmi|abbr=on}}, 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 {{convert|17|km|mi|abbr=on}} 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.{{cite journal |last1=Mustoe |first1=G. |year=2010 |title=Cyclic sedimentation in the Eocene Allenby Formation of south-central British Columbia and the origin of the Princeton Chert fossil beds |journal=Canadian Journal of Earth Sciences |volume=48 |issue=1 |pages=25–43 |doi=10.1139/e10-085}}{{cite journal |last1=Dillhoff |first1=R.M. |last2=Dillhoff |first2=T.A. |last3=Greenwood |first3=D.R. |last4=DeVore |first4=M.L. |last5=Pigg |first5=K.B. |year=2013 |title=The Eocene Thomas Ranch flora, Allenby Formation, Princeton, British Columbia, Canada |journal=Botany |volume=91 |issue=8 |pages=514–529 |doi=10.1139/cjb-2012-0313}}{{cite journal |last1=Greenwood |first1=D.R. |last2=Pigg |first2=K.B. |last3=Basinger |first3=J.F. |last4=DeVore |first4=M.L. |year=2016 |title=A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) Highlands floras of British Columbia, Canada, and Washington, U.S.A. |journal=Canadian Journal of Earth Sciences |volume=53 |issue=6 |pages=548–564 |doi=10.1139/cjes-2015-0177|bibcode=2016CaJES..53..548G |doi-access=free |hdl=1807/71961 |hdl-access=free }}
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" 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.{{cite journal |last1=Archibald |first1=S. |last2=Greenwood |first2=D. |last3=Smith |first3=R. |last4=Mathewes |first4=R. |last5=Basinger |first5=J. |year=2011 |title=Great Canadian Lagerstätten 1. Early Eocene Lagerstätten of the Okanagan Highlands (British Columbia and Washington State) |journal=Geoscience Canada |volume=38 |issue=4 |pages=155–164}}
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.{{Cite journal|last1=DeVore |first1=M. L. |last2=Nyandwi |first2=A. |last3=Eckardt |first3=W. |last4=Bizuru |first4=E. |last5=Mujawamariya |first5=M. |last6=Pigg |first6=K. B. |year=2020 |title=Urticaceae leaves with stinging trichomes were already present in latest early Eocene Okanogan Highlands, British Columbia, Canada |journal=American Journal of Botany |volume=107 |issue=10 |pages=1449–1456 |doi=10.1002/ajb2.1548 |pmid=33091153 |s2cid=225050834 |doi-access=free }}
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.{{cite book |last1=Penhallow |first1=D.P. |year=1908 |chapter=A report on Tertiary plants of British Columbia, collected by Lawrence M. Lambe in 1906 together with a discussion of previously recorded Tertiary floras |publisher=Canada Department of Mines, Geological Survey Branch |title=Report 1013 |pages=1–167}} Modern collecting has centered on the areas around One Mile Creek, Pleasant Valley, and Thomas Ranch.
Age
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).{{cite journal |last1=Shaw |first1=W. S. |year=1952 |title=The Princeton Coalfield, British Columbia. |journal=Geological Survey of Canada}}{{cite journal |last1=Arnold |first1=C. A. |year=1955 |title=A Tertiary Azolla from British Columbia |journal= Contributions from the Museum of Paleontology, University of Michigan |volume=12 |issue=4 |pages=37–45 |url= http://deepblue.lib.umich.edu/bitstream/2027.42/48289/2/ID129.pdf}} Half a decade later, the older age of {{mya|48|error=2|million years old}} was first suggested, with a younger age being suggested at {{mya|46.2|million years old|error=1.9}} in 2000 and an older date of {{mya|52.08|error=0.12}} obtained from uranium–lead dating of zircons from Vermilion Bluffs shale in 2005.
Lithology
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.
The coal seams throughout the formation are typically sub-bituminous.
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 {{convert|0.5-1|mm|in|abbr=on}} in modern temperate climates, this suggests the time needed for each {{convert|10-20|cm|in|abbr=on}} 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.
Palynoflora
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.
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.
| class="wikitable sortable" style="margin:auto; width:80%;" |
| Family
! Genus ! Species ! Pollen/Macrofossil ! Notes ! Images |
|---|
| Aquifoliaceae
| | | Pollen | A holly palynomorph | |
| Arecaceae
| | | Pollen | A palm palynomorph | |
| Buxaceae
| | †Erdtmanipollis pachysandroides | Pollen | A box family palynomorph | |
| Betulaceae
| | | Pollen & macrofossils | An alder palynomorph | |
| Betulaceae
| | | Pollen & macrofossils | A birch palynomorph | |
| Betulaceae
| | | Pollen | A hornbeam palynomorph | |
| Betulaceae
| | | Pollen | A hazelnut palynomorph | |
| Cupressaceae
| | | Pollen | A Cunninghamia like palynomorph | |
| Cupressaceae
| | | Pollen & macrofossils | A redwood palynomorph | |
| Cupressaceae
| | | Pollen & macrofossils | A Taxodioideae subfamily palynomorph | |
| Elaeagnaceae
| | | Pollen | An elaeagnaceous palynomorph, similar to oleaster | |
| Ericaceae
| unidentified | | Pollen | An ericaceous palynomorph of uncertain affinity | |
| Fagaceae
| | | Pollen | A chestnut palynomorph | |
| Fagaceae
| | | Pollen | A fagaceous palynomorph | |
| Fagaceae
| | | Pollen | A beech palynomorph | |
| Fagaceae
| | | Pollen | A beech palynomorph | |
| Fagaceae
| | | Pollen | A fagaceous palynomorph | |
| Fagaceae
| | | Pollen | An oak palynomorph, similar to Quercus Group Lobatae pollen | |
| Fagaceae
| | | Pollen | An oak palynomorph, ancestral type with Quercus Group Ilex morphology | |
| Fagaceae
| | | Pollen | A fagaceous palynomorph | |
| Fagaceae
| Unidentified | | Pollen | A Fagoideceous palynomorph | |
| Fagaceae
| | | Pollen | A fagaceous palynomorph, similar to oak | |
| Ginkgoaceae
| | | Pollen & macrofossils | A Gingko palynomorph | |
| Hamamelidaceae
| | | Pollen | A sweet gum palynomorph | |
| Juglandaceae
| | | Pollen | A hickory palynomorph | |
| Juglandaceae
| | | Pollen | A hickory palynomorph | |
| Lycopodiaceae
| | | Pollen | A lycopod palynomorph | |
| Malvaceae
| | | Pollen | A linden palynomorph | |
| Osmundaceae
| | | Pollen | An osmundaceous fern palynomorph | |
| Pinaceae
| | | Pollen & macrofossils | A fir palynomorph | |
| Pinaceae
| | | Pollen | A pine family palynomorph | |
| Pinaceae
| | | Pollen | A Picea palynomorph | |
| Pinaceae
| | | Pollen & macrofossils | A Pinus palynomorph | |
| Pinaceae
| | | Pollen | A pine family palynomorph | |
| Pinaceae
| | | Pollen & macrofossils | A Pseudolarix palynomorph | |
| Pinaceae
| | | Pollen | A Tsuga palynomorph | |
| Pinaceae
| | | Pollen | A Laricoidae palynomorph, similar to larch | |
| Pinaceae
| | | Pollen | A Laricoidae palynomorph, similar to pseudotsuga | |
| Platanaceae
| | | Pollen | A Platanus palynomorph | |
| Potamogetonaceae
| | | Pollen | A Potamogeton palynomorph | |
| Rosaceae
| Unidentified | | Pollen & macrofossils | Rose famnily palynomorphs | |
| Salicaceae
| | | Pollen | A willow palynomorph | |
| Salviniaceae
| | | Pollen & macrofossils | A duck weed palynomorph | |
| Sapindaceae
| | | Pollen & macrofossils | A maple palynomorph | |
| Sapindaceae
| | | Pollen & macrofossils | A horse chestnut palynomorph | |
| Sapotaceae
| Unidentified | | Pollen | A sapotaceous palynomorph | |
| Taxaceae
| | | Pollen | A yew palynomorph | |
| Ulmaceae
| | | Pollen & macrofossils | An elm palynomorph | |
| incertae sedis
| | †Pistillipollenites macgregorii | Pollen | A palynomorph of uncertain affinity, possibly a Gentianaceae or Euphorbiaceae species | |
Compression paleobiota
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.{{cite journal |last1=Kuc |first1=M. |year=1972 |title=Muscites eocenicus sp. nov.—a fossil moss from the Allenby Formation (middle Eocene), British Columbia |journal=Canadian Journal of Earth Sciences |volume=9 |issue=5 |pages=600–602 |doi=10.1139/e72-049|bibcode=1972CaJES...9..600K }}{{cite journal |last1=Kuc |first1=M. |year=1974 |title=Fossil mosses from the bisaccate zone of the mid-Eocene Allenby Formation, British Columbia |journal=Canadian Journal of Earth Sciences |volume=11 |issue=3 |pages=409–421 |doi=10.1139/e74-037|bibcode=1974CaJES..11..409K }} 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. Only two pteridophyte species have been described from the compression flora, Azolla primaeva by Penhallow (1890) and Equisetum similkamense by Dawson (1878).{{cite book |last1=Dawson |first1=J. W. |year=1890 |title=On fossil plants from the Similkameen Valley and other places in the southern interior of British Columbia. |publisher=Royal Society of Canada}}
The following fossil conifers, pteridophytes, ginkgophytes and bryophytes have been described from the Allenby Formation:
= Bryophytes=
| class="wikitable sortable" align="center" width="100%" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Amblystegiaceae
| | †Hypnites jovet-astiae{{cite book |last1=Miller |first1=N. G. |year=1980 |chapter=Fossil mosses of North America and their significance |title=The Mosses of North America |pages=9–36}} | (Kuc) Miller | An amblystegiaceous moss | |
| Amblystegiaceae
| | | (Kuc) Miller | An amblystegiaceous moss | |
| Bartramiaceae
| | | (Kuc) Miller | A bartramiaceous moss | |
| ?Ditrichaceae
| | | Kuc | | |
| incertae sedis
| | | Kuc | A moss of uncertain placement | |
| incertae sedis
| | | Kuc | A moss of uncertain placement | |
= Pteridophytes=
| class="wikitable sortable" align="center" width="100%" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Equisetaceae
| | | | | |
| Salviniaceae
| | | | A mosquito fern | |
=Gingkophytes=
| class="wikitable sortable" align="center" width="100%" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Ginkgoaceae
| | Ginkgo biloba{{cite journal |last1=Mustoe |first1=G.E. |year=2002 |title=Eocene Ginkgo leaf fossils from the Pacific Northwest |journal=Canadian Journal of Botany |volume=80 |issue=10 |pages=1078–1087 |doi=10.1139/b02-097}} | | A ginkgo | |
| Ginkgoaceae
| | | Mustoe, 2002 | A ginkgo with highly dissected leaves | |
=Pinophytes=
= Angiosperms =
=Mollusks=
| class="wikitable sortable" style="margin:auto; width:100%;" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Hydrobiidae
| | †Micropyrgus camselli{{cite journal |last1=Russell |first1=L. S. |year=1957 |title=Mollusca from the Tertiary of Princeton, British Columbia|journal=National Museum of Canada Bulletin |volume=147 |pages=84–95}} | L.S. Russell, 1957 | A hydrobiid mud snail | |
| Lymnaeidae
| | | L.S. Russell, 1957 | A lymnaeine pond snail | |
| Physidae
| | | L.S. Russell, 1957 | An aplexine bladder snail | |
| Physidae
| | | L.S. Russell, 1957 | A physine bladder snail | |
| Planorbidae
| | | L.S. Russell, 1957 | An ancylinine ramshorn snail | |
| Planorbidae
| | | L.S. Russell, 1957 | A possible planorbinine ramshorn snail | |
| Sphaeriidae
| | | L.S. Russell, 1957 | A possible sphaeriine fingernail clam | |
=Insects=
==Coleopterans==
==Dipterans==
==Hemipterans==
==Hymenopterans==
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 {{cvt|3.3|cm|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 {{cvt|5|cm|in}} length estimate, placing it as comparable to queens of T. lubei and T. simillima.{{cite journal |last1=Archibald |first1=S. |last2=Mathewes |first2=R. |last3=Aase |first3=A. |year=2023 |title=Eocene giant ants, Arctic intercontinental dispersal, and hyperthermals revisited: discovery of fossil Titanomyrma (Hymenoptera: Formicidae: Formiciinae) in the cool uplands of British Columbia, Canada |journal=The Canadian Entomologist |volume=155 |issue=e6|doi=10.4039/tce.2022.49 |s2cid=256598590 |doi-access=free }}
| class="wikitable sortable" style="margin:auto; width:100%;" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Braconidae
| | | | A braconid wasp | File:Bracon species 1890 pl3 Fig33.png sp. |
| Formicidae
| | | | A formiciine titan ant | file:Titianomyrma sp BBM-PAL-2022-00001 Allenby Formation Fig1a.png sp.]] |
| Ichneumonidae
| | | (Handlirsch, 1910) | A xoridine ichneumon parasitic wasp | |
| Tenthredinidae
| | †Eriocampa tulameenensis{{Cite journal |author=Rice, H.M.A. |title=Two Tertiary sawflies, (Hymenoptera - Tenthredinidae), from British Columbia |journal=Geological Survey of Canada |year=1968 |volume=67 |issue=59 |pages=1–21}} | Rice, 1968 | | File:Eriocampa tulameenensis holotype Rice 1968 Pl1 Fig1 cropped.png]] |
==Mecopterans==
==Neuropterans==
| class="wikitable sortable" style="margin:auto; width:100%;" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Ithonidae
| | †Ricaniella antiquata{{cite journal |last1=Meunier |first1=F. |year=1897 |title=Observations sur quelques insectes du Corallien de la Bavière |journal=Rivista Italiana di Paleontologia |volume=3 |pages=18–23}} | (Scudder, 1895) | A Polystoechotid-group giant lacewing{{cite journal |last1=Shcherbakov |first1=D. E. |year=2006 |title=The earliest find of Tropiduchidae (Homoptera: Auchenorrhyncha), representing a new tribe, from the Eocene of Green River, USA, with notes on the fossil record of higher Fulgoroidea |journal=Russian Entomological Journal |volume=15 |pages=315–322}} | File:Ricaniella antiquata Scudder 1895 pl1 Fig3.png |
==Odonata==
| class="wikitable sortable" style="margin:auto; width:100%;" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Aeshnidae
| Indeterminate | | | A daner dragonfly | |
| Cf. †Dysagrionidae
| | | Archibald & Cannings, 2022 | A possible Dysagrionidae odonate. | |
==Raphidiopterans==
| class="wikitable sortable" style="margin:auto; width:100%;" |
| Family
! Genus ! Species ! Authority ! Notes ! Images |
|---|
| Raphidiidae
| | †Megaraphidia hopkinsi{{Cite journal|last1=Archibald |first1=S. B. |last2=Makarkin |first2=V. N. |title=Early Eocene snakeflies (Raphidioptera) of western North America from the Okanagan Highlands and Green River Formation |year=2021 |journal=Zootaxa |volume=4951 |issue=1 |pages=41–79 |doi=10.11646/zootaxa.4951.1.2 |pmid=33903413 |s2cid=233411745 }} | Archibald & Makarkin, 2021 | | |
=Vertebrates=
Princeton Chert biota
{{main|Princeton chert}}
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.{{cite journal |last1=Pigg |first1=K. B. |last2=DeVore |first2=M. L. |year=2016 |title=A review of the plants of the Princeton chert (Eocene, British Columbia, Canada) |journal=Botany |volume=94 |issue=9 |pages=661–681 |doi=10.1139/cjb-2016-0079|hdl=1807/73571 |hdl-access=free }}
=Fungi=
=Ferns=
=Conifers=
=Angiosperms=
References
{{Reflist|30em}}
{{commons category|Allenby Formation}}
Category:Sandstone formations of Canada