Acer ferrignoi Temporal range: | |
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Scientific classification | |
Kingdom: | Plantae |
Clade: | Tracheophytes |
Clade: | Angiosperms |
Clade: | Eudicots |
Clade: | Rosids |
Order: | Sapindales |
Family: | Sapindaceae |
Genus: | Acer |
Section: | Acer sect. Rubra |
Species: | †A. ferrignoi |
Binomial name | |
†Acer ferrignoi Wolfe & Tanai, 1987 | |
Acer ferrignoi is an extinct maple species in the family Sapindaceae described from a group of fossil leaves. The species is known from Miocene sediments exposed in Oregon, US. It is one of several extinct species belonging to the living section Rubra .
Acer ferrignoi is known from a small group of fossils from a late Miocene fossil site listed as USGS 9737. The site is located near Lolo Pass in the northern Oregon Cascade mountains. [1] The fossils were first studied by paleobotanists Jack A. Wolfe of the United States Geological Survey, Denver office and Toshimasa Tanai of Hokkaido University. They determined that fossils belonged to an undescribed Acer section Eriocarpa species. Wolfe and Tanai published their 1987 type description for A. ferrignoi in the Journal of the Faculty of Science, Hokkaido University. [1] The etymology of the chosen specific name ferrignoi is in recognition of James P. Ferrigno, who located and supplied access to collections of fossils housed in the Smithsonian Institutions National Museum of Natural History. [1] At the time of description the A. ferrignoi holotype specimen, number NMNH 396125, along with the four paratypes were part of the National Museum of Natural History collections. [1]
Wolfe and Tanai suggested A. ferrignoi may be a late Miocene descendant of Acer chaneyi which lived from the late Oligocene to the Middle Miocene before going extinct. While A. cheneyi leaves sometimes have three lobes as in A. ferrignoi, more often they were five lobed, which is not seen in A. ferrignoi. The similarity in the structure and concave outlines between the two species' lateral lobes were major factors in Wolfe and Tanai's suggestion of relation between the two species. Following the Acer taxonomy structure defined by Japanese botanist Ken Ogata, they placed the species and related fossils into the Acer section Eriocarpa. Later work on the systematics of the genus resulted in section Eriocarpa being included into section Rubra. [2]
Leaves of Acer ferrignoi are simple in structure, with perfectly actinodromous vein structure and range from ovate to widely ovate in shape. [1] The base of each leaf is rounded, with the petiole ranging up to 0.5 cm (0.20 in). The leaves are dissected into three lobes, with the lateral lobes being one-half to three-quarters as long as the median lobe. The median lobe is generally triangular in outline and the two lateral lobes are narrow and triangular. There are three primary veins with between three and ten secondary veins branching off from the outer primaries. The secondary veins branch from the primaries at angles of 40° to 70° and run straight to the margins or arch gradually with external vein forks that reach the margins. [1]
Acer douglasense is an extinct maple species in the family Sapindaceae described from fossil leaves. The species is solely known from the Early Eocene sediments exposed in Katmai National Park and Preserve, Kodiak Island Borough, Alaska. It is the type species for the extinct section Douglasa.
Acer alaskense is an extinct maple species in the family Sapindaceae described from a fossil leaf. The species is solely known from the Latest Paleocene sediments exposed in the Matanuska River Valley, Matanuska-Susitna Borough, Alaska. It is the type species for the extinct section Alaskana.
Acer stewarti is an extinct maple species in the family Sapindaceae described from a series of fossil leaves and samaras. The species is solely known from the Early Eocene sediments exposed in south central British Columbia, Canada adjacent to northeast Washington state, United States. It is one of only two species belonging to the extinct section Stewarta.
Acer browni is an extinct maple species in the family Sapindaceae described from a series of isolated fossil leaves and samaras. The species is known from the early to middle Miocene sediments exposed in Western Oregon, Washington state, USA and Northern Graham Island, Haida Gwaii, Canada. It is one of several extinct species placed in the living section Parviflora.
Acer smileyi is an extinct maple species in the family Sapindaceae described from a series of isolated fossil leaves and samaras. The species is known from the late Oligocene to middle Miocene sediments exposed in the states of Alaska, Idaho, Nevada, and Oregon, USA. It is one of several extinct species placed in the living section Parviflora.
Acer ashwilli is an extinct maple species in the family Sapindaceae described from a group of fossil leaves and samaras. The species is solely known from the Early Oligocene sediments exposed in central Oregon, USA. It is one of several extinct species belonging to the living section Ginnala.
Acer clarnoense is an extinct maple species in the family Sapindaceae described from a series of isolated fossil leaves and samaras. The species is known from the late Eocene sediments exposed in the state of Oregon in the US. It is one of several extinct species placed in the living section Macrantha.
Acer dettermani is an extinct maple species in the family Sapindaceae described from a series of isolated fossil leaves. The species is known from the late Eocene to early Oligocene sediments exposed in the state of Alaska, USA. It is one of several extinct species placed in the living section of Macrantha.
Acer castorrivularis is an extinct maple species in the family Sapindaceae described from a solitary fossil leaf. The species is known from the latest Eocene sediments exposed in the state of Montana, USA. It is one of several extinct species placed in the living section Macrantha.
Acer latahense is an extinct maple species in the family Sapindaceae described from series of isolated fossil leaves. The species is known from the latest early to middle Miocene sediments exposed in the states of Oregon and Washington, USA. It is one of several extinct species placed in the living section Macrantha.
Acer palaeorufinerve is an extinct maple species in the family Sapindaceae described from series of isolated fossil samaras and leaves. The species was described from Miocene to Pliocene aged fossils found in Japan and is known from Korean fossils and Miocene sediments exposed in the state of Alaska, USA. It is one of several extinct species placed in the living section Macrantha.
Acer traini is an extinct maple species in the family Sapindaceae described from isolated fossil samaras. The species was described from Miocene-aged fossils found in Canada and the United States of America. It is one of several extinct species placed in the living section Glabra.
Acer ivanofense is an extinct maple species in the family Sapindaceae described from series of isolated fossil leaves. The species was described from Eocene to Oligocene aged fossils found in the United States of America. It is one of several extinct species placed in the living section Glabra.
Acer taurocursum is an extinct maple species in the family Sapindaceae described from a single fossil samara found in Late Eocene lakebed sediments exposed in the state of Nevada, US. It is one of several extinct species placed in the living section Rubra.
Acer kenaicum is an extinct maple species in the family Sapindaceae described from a pair of fossil leaves and a samara. The species is known solely from the Oligocene sediments found exposed in central coastal Alaska, US. It is one of several extinct species belonging to the living section Rubra.
Acer chaneyi is an extinct maple species in the family Sapindaceae described from a number of fossil leaves and samaras. The species is known from Oligocene to Miocene sediments exposed in Alaska, Idaho, Nevada, Oregon and Washington in the U.S. It is one of several extinct species belonging to the living section Rubra.
Acer whitebirdense is an extinct maple species in the family Sapindaceae described from a number of fossil leaves and samaras. The species is known from Miocene sediments exposed in Idaho, Oregon and Washington in the United States. It is one of several extinct species belonging to the living section Rubra.
Acer taggarti is an extinct maple species in the family Sapindaceae described from a number of fossil leaves and samaras. The species is known from Miocene sediments exposed in central Oregon, US. It is one of several extinct species belonging to the living section Rubra.
Acer lincolnense is an extinct maple species in the family Sapindaceae described from a group of fossil leaves and fruits. The species is known from Eocene sediments exposed in the US state of Montana. It is tentatively placed into the living Acer section Cissifolia.
Trochodendron rosayi is an extinct species of flowering plant in the family Trochodendraceae. The species is known from fossils found in Middle Miocene deposits of central Oregon. T. rosayi are possibly the fruits belonging to the extinct trochodendraceous leaf species Trochodendron postnastae.