Kardiasperma

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Kardiasperma
Temporal range: Middle Eocene, 45–43 Mya
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Scientific classification OOjs UI icon edit-ltr.svg
Kingdom: Plantae
Clade: Tracheophytes
Clade: Angiosperms
Clade: Eudicots
Clade: Rosids
Order: Fagales
Family: Betulaceae
Subfamily: Coryloideae
Genus: Kardiasperma
Manchester
Species:
K. parvum
Binomial name
Kardiasperma parvum
Manchester

Kardiasperma is an extinct genus of flowering plants in the hazelnut family, Betulaceae, containing the single species Kardiasperma parvum. [1] The species is solely known from the middle Eocene sediments exposed in north central Oregon and was first described from a series of isolated fossil nuts in cherts. [1]

Contents

History and classification

Kardiasperma parvum has been identified from a single location in the Clarno Formation, the Clarno nut beds, type locality for both the formation and the species. The nut beds are approximately 3 kilometres (1.9 mi) east of the unincorporated community of Clarno, Oregon, and currently considered to be middle Eocene in age, based on averaging zircon fission track radiometric dating which yielded an age of 43.6 and 43.7 ± 10 million years ago and argon–argon dating radiometric dating which yielded a 36.38 ± 1.31 to 46.8 ± 3.36 Mya date. [1] The average of the dates resulted in an age range of 45 to 43 Mya. The beds are composed of silica and calcium carbonate cemented tuffaceous sandstones, siltstones, and conglomerates which preserve either a lake delta environment, or alternatively periodic floods and volcanic mudflows preserved with hot spring activity. [1]

The genus and species was described from a series of type specimens, the holotype specimen USNM 435077, which is currently preserved in the paleobotanical collections of the National Museum of Natural History in Washington, D.C., and thirty-seven paratype specimens. Eighteen of the paratypes are also in the national Museum collections, while three are in the University of Florida collections, and the remaining four specimens are part of the University of California Museum of Paleontology. The fossils were part of a group of approximately 20,000 specimens collected from 1942 to 1989 by Thomas Bones, Alonzo W. Hancock, R. A. Scott, Steven R. Manchester, and a number of high school students. [1]

The Kardiasperma specimens were studied by paleobotanist Steven R. Manchester of the University of Florida. He published his 1994 type description for K. parvum in the journal Palaeontographica Americana . [1] In his type description Manchester noted the generic name is derived from the Greek words Kardia meaning "heart" and sperma meaning "seed". The specific epithet parvum, Latin for "small, was chosen in reference to the small size of the locule casts. [1] The fossils are noted to be nearly identical to fossils of the related and also extinct Betulaceae genus Palaeocarpinus from North Dakota. The two genera are separated on the basis of the notable size difference between the Palaeocarpinus and Kardiasperma fossils and the lack of a surrounding bract on the Kardiasperma. [1]

Description

The locules of Kardiasperma parvum are generally obcordate, with quadrilateral symmetry, a rounded base and a bluntly pointed apex. The locules have an overall length ranging between 1.3–2.4 millimetres (0.051–0.094 in) and a maximum width between 1.0 to 2.0 millimetres (0.039 to 0.079 in). The exterior surface has a smooth texture and a keel running along the major plane of symmetry, while a groove runs along the middle of the locule along the minor plane of symmetry from the base to the apex. [1]

Related Research Articles

Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 1954.

Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 1940.

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<i>Corylopsis reedae</i> Extinct species of flowering plant

Corylopsis reedae is an extinct species of flowering plant in the family Hamamelidaceae known from fossil leaves found in the early Eocene Klondike Mountain Formation deposits of northern Washington state. C. readae is one of the oldest occurrences of the winter-hazel genus Corylopsis, which includes between seven and thirty species, all found in Asia. Fossils from two other occurrences are of similar age to C. readae, with Paleocene specimens from Greenland being placed in the form taxon Corylopsiphyllum and an Eocene Alaskan fossil being included in Corylopsis without species placement.

Taxus masonii is an extinct species of conifer in the yew family, Taxaceae, solely known from the middle Eocene sediments exposed in north central Oregon. The species was first described from a series of isolated fossil seeds in chert.

Torreya clarnensis is an extinct species of conifer in the yew family Taxaceae solely known from the middle Eocene sediments exposed in north central Oregon. The species was first described from a series of isolated fossil seeds in chert.

Diploporus is an extinct genus of conifers in the yew family Taxaceae, containing the single species Diploporus torreyoides known from the middle Eocene of north central Oregon and the Late Paleocene of south central North Dakota. The species was first described from a series of isolated fossil seeds in chert.

Actinidia oregonensis is an extinct species of flowering plants in the kiwifruit family, Actinidiaceae, solely known from the middle Eocene sediments exposed in north-central Oregon. The species was first described from a series of isolated fossil seeds in chert.

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Paleopanax is an extinct genus of flowering plant in the Ginseng and Ivy family, Araliaceae, containing the single species Paleopanax oregonensis. The species is solely known from the middle Eocene sediments exposed in north central Oregon and was first described from a series of isolated fossil fruits in siltstones.

Coryloides is an extinct genus of flowering plants in the hazelnut family, Betulaceae, containing the single species Coryloides hancockii. The species is solely known from the middle Eocene sediments exposed in north central Oregon and was first described from a series of isolated fossil nuts in cherts.

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References

  1. 1 2 3 4 5 6 7 8 9 Manchester, S.R. (1994). "Fruits and Seeds of the Middle Eocene Nut Beds Flora, Clarno Formation, Oregon". Palaeontographica Americana. 58: 30–31.