''Microsyops'' is a
plesiadapiform primate found in Middle
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...
in
North America. It is in the family
Microsyopidae, a
plesiadapiform family characterized by distinctive lanceolate lower first incisors.
It appears to have had a more developed sense of smell than other early primates. It is believed to have eaten fruit, and its fossils show the oldest known dental
cavities in a
mammal.
There are nine species of ''Microsyops'' that exist in the fossil record from the middle
Wasatchian (~53 million years ago) through
Uintan
The Uintan North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages
The North American land mammal ages (NALMA) establishes a geologic timescale for North American fauna b ...
(~42 million years ago) North American Land Mammal Ages. ''Microsyops'' is primarily known from the
Rocky Mountain region of the
United States
The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 U.S. state, states, a Washington, D.C., federal district, five ma ...
, though fossils have also been found in
California
California is a state in the Western United States, located along the Pacific Coast. With nearly 39.2million residents across a total area of approximately , it is the most populous U.S. state and the 3rd largest by area. It is also the ...
and
Texas
Texas (, ; Spanish language, Spanish: ''Texas'', ''Tejas'') is a state in the South Central United States, South Central region of the United States. At 268,596 square miles (695,662 km2), and with more than 29.1 million residents in 2 ...
.
Diet and body size
Body size diversity of ''Microsyops'' spans from the 700-gram ''Microsyops cardiorestes'' to over 3000 grams for ''Microsyops kratos,'' estimated using the dimensions of the upper and lower last premolar and first molar.
The diet of ''Microsyops'' is varied among the nine species, with the smaller-bodied and more primitive species, like ''M. cardiorestes'', likely able to exist by eating almost exclusively insects.
[ However, larger-bodied species, such as ''Microsyops annectens'' or ''M. kratos'', likely needed to expand their diets to include other food sources. This is also supported by wear facets on the molars of ''M. annecten''s and ''M. kratos'' that are indicative of heavier shearing and crushing forces required of harder foods like fruits and nuts.][ Another indication of expanded diets, away from strict insectivory, comes in the form of reported cavities in a sample of ''Microsyops latidens'' where a sample of 1030 individuals included 77 specimens showing signs of cavities. In this case, cavities are likely caused by a reliance on more sugary foods, such as fruits, moving away from strict insectivory.
]
Morphology
Dental morphology
Consistent with other North American members of Microsyopidae, ''Microsyops'' has a lower central incisor that is enlarged, procumbent, and lanceolate. The expansive flattened surface of the lower central incisor is oriented towards the front of the tooth. ''Microsyops'' has a lower dental formula of 1-0-3-3, with one incisor, no canine, three premolars, and three molars. The lower second premolar is single-rooted, and the third premolar is premolariform. The fourth lower premolar has a distinct metaconid, no paraconid, and a two-cusped talonid with a more fully-developed basin than in the closely related ''Arctodontomys''. Lower molars each have a small yet distinct paraconid, a semi-compressed trigonid, a developed mesoconid, and a small, twinned hypoconulid.[
The upper canine of ''Microsyops'' is double-rooted. The upper fourth premolar has a distinct metacone and a weak parastyle. Upper molars exhibit clear conules, in particular a distinct metaconule, unlike the condition in the closely related ''Craseops''.][ Additionally, ''Microsyops'' upper molars lack a postprotocingulum, in contrast to the condition found in most early ]Paleogene
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of ...
primates.[
]
Cranial and postcranial morphology
The basicranium of ''Microsyops'' has been described in detail in order to determine its affinities with respect to other mammals. Based on basicranial features, the internal carotid artery which supplied blood to the brain of ''Microsyops'' was primitive with respect to both extinct and extant euarchontans. These features include a transpromontorial groove indicating an unreduced internal carotid artery and grooves marking the course for both stapedial and promontorial branches of the internal carotid artery (Silcox et al. 2020). Another characteristic that suggests Microsyops was primitive is the presence of unexpanded caudal and rostral tympanic petrosal processes.[ Unlike other plesiadapiforms, ''Microsyops'' lacked a bony auditory bulla (Gunnel 1989, Silcox et al. 2020). Additionally, ''Microsyops'' lacks the specialized cranial morphology considered characteristic of crown scandentians and dermopterans.]
The most characteristic aspect of the cranial morphology of Microsyops is the presence of a postorbital process.[ This trait is unlike the condition found in early Paleogene primates, which possess a full postorbital bar. However, Microsyops also differs from other plesiadapiforms, which lack either a postorbital bar or process.][ The postorbital process of ''Microsyops'' has been described as being superficially similar to that of dermopterans.][
Due to limited available material, very little is known about the postcranial morphology of ''Microsyops'', and Microsyopidae in general.][
]
Taxonomy
''Microsyops'' was first described by Joseph Leidy
Joseph Mellick Leidy (September 9, 1823 – April 30, 1891) was an American paleontologist, parasitologist and anatomist.
Leidy was professor of anatomy at the University of Pennsylvania, later was a professor of natural history at Swarthmore ...
in 1872. He compared lower jaw fragments, found by Dr. J. V. Carter in the Bridger Basin of southwestern Wyoming
Wyoming () is a state in the Mountain West subregion of the Western United States. It is bordered by Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the sou ...
, to the condylarth ''Hyopsodus gracilis'', named by Professor O. C. Marsh
Othniel Charles Marsh (October 29, 1831 – March 18, 1899) was an American professor of Paleontology in Yale College and President of the National Academy of Sciences. He was one of the preeminent scientists in the field of paleontology. Among h ...
of Yale University
Yale University is a Private university, private research university in New Haven, Connecticut. Established in 1701 as the Collegiate School, it is the List of Colonial Colleges, third-oldest institution of higher education in the United Sta ...
. At the time he believed the fragments to represent the same animal and proposed the new binomial combination of ''Microsyops gracilis''. Leidy later compared his ''M. gracilis'' to Marsh's ''Limnotherium elegans'', which was originally described as a diminutive mammal and later as a primate. He concluded they were the same but with L. elegans as a species of the genus Microsyops, and that his original Microsyops gracilis should be properly named Microsyops elegans.[
Microsyopinae and Uintasoricinae are subfamilies within the plesiadapiform family Microsyopidae. ''Microsyops'' is a genus of the subfamily Microsyopinae which also includes the genera ''Arctodontomys'', ''Megadelphus'' and ''Craseops''. This subfamily includes the larger microsyopids. The subfamily Uintasoricinae includes the diminutive taxa ''Niptomomys'', ''Uintasorex'', and ''Choctawius''. Microsyopidae is one of the longest-lived groups of plesiadapiforms, lasting 20 million years in North America from the late Paleocene to late Eocene (Silcox et al. 2021). Two families of plesiadapiforms, Microsyopidae and Paromomyidae, have representative taxa from the Uintan Land-Mammal Age (middle Eocene) while the Plesiadapidae and Carpolestidae disappeared at the end of the Paleocene.]
Recognized species of Microsyops includes ''M. elegans'', ''M. annectens'', ''M. scottianus'', ''M. augustidens'', ''M. kratos'', ''M. latidens'', ''M. cardiorestes'', ''M. vicarius'', and ''M. knightensis,'' with ''M. elegans'' being the type species.[
Some authors argue that microsyopids are plesiadapiforms while others suggest a dermopteran grouping.] However, the overall relationship between plesiadiforms and other living and fossil members of Euarchontoglires has been disputed. In a cladistic analysis including postcranial, cranial, and dental characteristics by Bloch et al. (2007), microsyopids were found to be plesiadapiforms more distantly related to euprimates than plesiadapoids or paromomyoids, and without any special relationship to dermopterans.[ However, while analyses support a euarchontan grouping, specific relationships of microsyopids to other plesiadapiforms, euprimates, scandentia, and dermoptera remain unresolved.][ Microsyopids are generally thought to be euarchontans, and some researchers consider them to be stem primates.]
Paleoenvironment
Microsyopidae lived from the late Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch that lasted from about 66 to 56 million years ago (mya). It is the first epoch of the Paleogene Period in the modern Cenozoic Era. The name is a combination of the Ancient Greek ''pal ...
to the middle Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...
in North America.[ Conditions of the ]Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...
supported extensive subtropical woodland and rainforest environments which facilitate arboreal
Arboreal locomotion is the locomotion of animals in trees. In habitats in which trees are present, animals have evolved to move in them. Some animals may scale trees only occasionally, but others are exclusively arboreal. The habitats pose num ...
lifestyles. This time is also characterized by the Paleocene-Eocene Thermal Maximum, displaying the highest temperatures of the Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configu ...
period. From this peak, steady temperature declines are displayed throughout the middle to late Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...
.
Notable fossils
A well-preserved skull of ''Microsyops annectens'' from Carter Mountain in northwestern Wyoming
Wyoming () is a state in the Mountain West subregion of the Western United States. It is bordered by Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the sou ...
has been used to generate a virtual endocast
An endocast is the internal cast of a hollow object, often referring to the cranial vault in the study of brain development in humans and other organisms. Endocasts can be artificially made for examining the properties of a hollow, inaccessible sp ...
via micro-CT
X-ray microtomography, like tomography and X-ray computed tomography, uses X-rays to create cross-sections of a physical object that can be used to recreate a virtual model ( 3D model) without destroying the original object. The prefix '' micr ...
.[ Cranial capacity has been estimated as 5.9 cm, yielding an ]encephalization quotient
Encephalization quotient (EQ), encephalization level (EL), or just encephalization is a relative brain size measure that is defined as the ratio between observed to predicted brain mass for an animal of a given size, based on nonlinear regressi ...
(EQ) of 0.26-0.52 depending on different body mass estimates and the choice of equation used to estimate EQ. ''Microsyops'' has larger EQ than '' Plesiadapis cookei'', and falls in the lower range of estimates for early Paleogene primates. However, basicranial anatomy is remarkably primitive, because the auditory bulla
The tympanic part of the temporal bone is a curved plate of bone lying below the squamous part of the temporal bone, in front of the mastoid process, and surrounding the external part of the ear canal.
It originates as a separate bone (tympani ...
was not ossified and there are only grooves, rather than bony tubes, for the intrabullar parts of the internal carotid artery and its dependencies.[ The basicranial anatomy of ''Microsyops'' appears to be little changed from that of primitive ]placental
Placental mammals (infraclass Placentalia ) are one of the three extant subdivisions of the class Mammalia, the other two being Monotremata and Marsupialia. Placentalia contains the vast majority of extant mammals, which are partly distinguishe ...
mammals.
References
{{Taxonbar, from=Q28455296
Plesiadapiformes
Prehistoric primate genera
Eocene primates
Ypresian life
Lutetian life
Bartonian life
Wasatchian
Bridgerian
Uintan
Eocene mammals of North America
Fossils of the United States
Paleontology in California
Paleontology in Colorado
Paleontology in Montana
Paleontology in New Mexico
Paleontology in North Dakota
Paleontology in Texas
Paleontology in Utah
Paleontology in Wyoming
Fossil taxa described in 1872
Taxa named by Joseph Leidy