quadgram

This is a table of type quadgram and their frequencies. Use it to search & browse the list to learn more about your study carrel.

quadgram frequency
museum of natural history57
extension of premaxillae posterior49
of premaxillae posterior to49
premaxillae posterior to nasals48
in every measurement taken46
topotypes of thomomys bottae38
alveolar length of upper30
from the type locality29
of m and m27
from those of thomomys25
university of kansas lawrence25
university of kansas publications24
smaller in every measurement24
length of hind foot24
of upper molar series23
length of upper molar23
zygomatic processes of maxillae21
those of thomomys bottae20
with topotypes of thomomys20
can be distinguished from20
larger in every measurement20
pocket gophers of the20
compared with topotypes of19
the posterior wall of18
distinguished from those of18
at the edge of17
posterior ends of nasals17
from topotypes of thomomys17
the first and second16
final stages of wear16
tympanic bullae more inflated16
of the tribe geomyini16
see accounts of those16
half of tail white16
posterior tongues of premaxillae16
tail and hind foot16
the type locality of16
known only from the16
in m and m16
of the great plains16
posterior wall of p15
hind feet and distal15
length of maxillary tooth15
first and second molars15
the anterior and posterior15
mastoid processes of squamosal14
claws on front feet14
on the basis of14
posterior to nasals less13
publications museum of natural13
across mastoid processes of13
and more nearly flat13
kansas publications museum of13
united states national museum13
of kansas publications museum13
posterior wall of m13
near topotypes of thomomys13
accounts of those forms13
and hind foot shorter12
of the genus thomomys12
part of the state12
upper incisors longer and12
topotypes of thomomys talpoides12
gophers of the genus12
of natural history volume12
be distinguished from those12
kansas lawrence university of11
a new pocket gopher11
the edge of the11
of the virgin river11
and zygomatic process of11
the early and middle11
more ochraceous and less11
they are here referred11
lawrence university of kansas11
distal half of tail11
the university of kansas11
of kansas lawrence university11
of the cheek teeth11
of natural history editors11
of thomomys bottae albicaudatus10
jugal and zygomatic process10
posterior to nasals greater10
on posterior wall of10
interpterygoid space narrowly v10
for comparisons with thomomys10
bullae more inflated ventrally10
union of jugal and10
arches more widely spreading10
and top of head10
to which they are10
of the first and10
front and hind feet10
which they are here10
on the posterior wall10
of jugal and zygomatic10
the final stages of10
as well as relatively10
ascending processes of premaxillae10
zygomatic arches more widely10
in the early miocene9
in the vicinity of9
more precise than county9
no locality more precise9
kansas printed by ferd9
in the late pliocene9
of the posterior loph9
walls of m and9
zygomata more widely flaring9
actually as well as9
upper incisors long and9
species of the genus9
zygomatic process of maxilla9
the base of the9
printed by ferd voiland9
in the final stages9
of thomomys bottae centralis9
on the sides of9
shaped as opposed to9
locality more precise than9
in the living species9
of approximately the same9
of the university of9
plate on posterior wall9
of the pocket gophers9
initial stages of wear9
hind foot basilar length8
alveolar length of maxillary8
nasals zygomatic breadth mastoid8
total length length of8
to nasals length of8
of hind foot basilar8
space more narrowly v8
molar series extension of8
of tail length of8
zygomata less widely flaring8
extension of premax post8
the occlusal surface of8
breadth alveolar length of8
the shape of the8
upper molar series extension8
sides and flanks to8
length of tail length8
interpterygoid space more narrowly8
larger and more inflated8
on the lingual side8
and hind feet and8
breadth interorbital breadth alveolar8
foot basilar length length8
of rostrum breadth of8
of the subfamily geomyinae8
approximately the same size8
to the north and8
breadth mastoid breadth interorbital8
side of the tooth8
length length of nasals8
on the occlusal surface8
postauricular patches small and8
of nasals zygomatic breadth8
only from the type8
zygomatic breadth mastoid breadth8
posterior walls of m8
from the vicinity of8
width across mastoid processes8
tail length of hind8
rostrum breadth of rostrum8
interorbital breadth alveolar length8
differ from those of8
the initial stages of8
of thomomys bottae aureiventris8
length length of tail8
length of rostrum breadth8
enamel plate on posterior8
basilar length length of8
series extension of premax8
length of nasals zygomatic8
inguinal and pectoral regions8
of the two columns8
comparisons with thomomys bottae8
mastoid breadth interorbital breadth8
inhabited by pocket gophers8
nasals length of rostrum8
more buffy and less7
bullae well inflated ventrally7
to length of skull7
new pocket gophers of7
the posterior enamel plate7
the western united states7
of geomys from the7
zygomatic arches weaker and7
standards and color nomenclature7
third to half of7
is considered to be7
the breadth across the7
anterior and posterior columns7
at edge of protomeres7
in the late pleistocene7
from the late pliocene7
the sides of the7
tympanic bullae well inflated7
posteriorly as opposed to7
and posterior enamel plates7
the saw rock canyon7
to half of tail7
color standards and color7
anterior and posterior enamel7
to the east and7
american museum of natural7
upper incisors shorter and7
size smaller in every7
the rexroad local fauna7
of the early miocene7
among named races of7
in the united states7
upper parts cinnamon buff7
from near topotypes of7
thomomys perpallidus aureus bailey7
postauricular patches larger and7
tympanic bullae larger and7
the edge of their7
of wear on the7
in the majority of7
of wear in the7
enamel plate on the7
the majority of characters7
final stage of wear7
the geographic range of7
distal third to half7
in the lower teeth7
the modern pocket gophers7
anterior and posterior walls7
of the late pleistocene7
posterior wall of the7
tympanic bullae moderately inflated7
phyletic development of the7
distal part of tail6
revision of the pocket6
into a single column6
the posterior loph is6
the lingual side of6
postauricular patches smaller and6
both anterior and posterior6
and distal part of6
early and middle pleistocene6
topotypes of cratogeomys castanops6
of the united states6
of thomomys bottae absonus6
extension of supraoccipital posterior6
of the late pliocene6
from north to south6
in the final stage6
on the great plains6
mastoid and tympanic bullae6
enamel on the posterior6
buis ranch local fauna6
the museum of natural6
pointed out that the6
stages of wear in6
part of tail white6
the colorado plateau province6
that part of the6
edge of their protomeres6
found to the north6
the anterior face of6
wear on the occlusal6
postauricular patches grayish black6
color of upper parts6
both above and below6
zygomatic arches heavier and6
of enamel on the6
of supraoccipital posterior to6
is limited to the6
the northern part of6
races of thomomys bottae6
posterior margins of nasals6
the structure of the6
of the upper incisor6
to be intergrades between6
at union of jugal6
bullae larger and more6
to the west and6
those of thomomys talpoides6
occlusal surface of the6
tympanic bullae less inflated6
of the skull is6
the central plateau of6
named races of thomomys6
found to the east6
upper incisors projecting anteriorly6
natural history of the6
and posterior walls of6
patches smaller and lighter6
early and middle miocene6
can be readily distinguished6
text is shown within6
and more inflated ventrally6
the sequence of wear6
of thomomys talpoides uinta6
the living species of6
union of the two6
found to the south6
the posterior surface of6
loss of enamel from6
from topotypes of cratogeomys6
the pocket gophers of6
and shape of the5
least depth of rostrum5
final stages of attrition5
the late pliocene and5
and less inflated ventrally5
posterior to lambdoidal suture5
length of upper maxillary5
the west side of5
of adult males of5
is restricted to the5
supraoccipital posterior to lambdoidal5
posterior part of the5
subspecies of thomomys talpoides5
pleisothomomys gidley and gazin5
and distal half of5
kansas museum of natural5
lingual side of the5
the final stage of5
closely allied to the5
the sangre de cristo5
reduction of enamel on5
patches larger and darker5
posterior to nasals long5
in western north america5
the main line of5
from the early and5
the subspecies to the5
zygomatic and mastoidal breadths5
in the shape of5
arches heavier and more5
in the museum of5
it seems unlikely that5
genera of the tribe5
topotypes and near topotypes5
of the zygomatic arches5
posterior extensions of premaxillae5
top of head dusky5
occipitonasal length of skull5
on the other hand5
talpoides uinta as follows5
to the west of5
m and m are5
late pliocene to recent5
the third upper molar5
species of the subgenus5
in the early pleistocene5
but are referable to5
as low as feet5
of head grayish black5
more rufous and less5
incisors long and narrow5
cheeks and top of5
least width of braincase5
in all stages of5
on front feet longer5
saw rock canyon local5
of adult females of5
and distal third to5
in the university of5
long axis of the5
of the genus geomys5
rostrum long and narrow5
greatest height of cranium5
the end of the5
the kansas university endowment5
top of head grayish5
has been reported from5
feet and distal third5
upper and lower molars5
the united states national5
the posterior face of5
kansas university endowment association5
both upper and lower5
posterior border of nasals5
be readily distinguished from5
the biological surveys collection5
northern part of the5
corner of the state5
of the posterior enamel5
for the loan of5
thomomys talpoides uinta as5
mastoid bullae less inflated5
of upper maxillary tooth5
and hind feet white5
pinkish buff on underparts5
to differ as follows5
curtis ranch local fauna5
one or the other5
in the subfamily geomyinae5
is known only from5
rock canyon local fauna5
as a result of5
and less widely spreading5
masseteric ridge and fossa5
the two columns of5
wall of the tooth5
all stages of wear5
the evolution of the5
closely resemble those of5
from san josecito cave5
on the central plateau5
from zion national park5
anterior face of the5
m and m of5
show them to be5
per cent of the5
the posterior part of5
subspecies of thomomys bottae5
of posterior wall of5
size larger in every5
measurements of adult males5
are referable to the5
the pattern of wear5
of the subgenus pappogeomys5
bullae moderately inflated ventrally5
more closely allied to5
finely mixed with black5
over sides and flanks5
part of the range5
across the zygomatic arches5
see account of that5
measurements of adult females5
the sevier river valley5
face of the upper5
one of the most5
markedly smaller in every4
them to be of4
wyoming and colorado by4
the enamel plates are4
of the posterior wall4
in the upper teeth4
grading over sides and4
the southern part of4
late pliocene and early4
the southwestern united states4
southern rocky mountain province4
patches small and dusky4
variation in the pocket4
thomomys talpoides occurring in4
smiths valley local fauna4
can be distinguished by4
the ends of the4
and more widely spreading4
for a railroad route4
attenuatus differs in smaller4
wall of m and4
of the subgenus cratogeomys4
the southeastern united states4
c d e f4
to the pacific ocean4
railroad route from the4
processes of maxillae heavier4
the mississippi river to4
or the other of4
the san luis valley4
of the posterior plate4
the pleistocene lake bonneville4
stage of wear in4
gophers of the subfamily4
the level of the4
the buis ranch local4
plate on the posterior4
of natural history of4
ears longer and more4
arches weaker and less4
sides of each column4
tongues of premaxillae narrower4
the skull of the4
the range here ascribed4
widely spreading and angular4
adult males of thomomys4
but differs as follows4
zygomatic processes of squamosals4
upper incisors short and4
on inguinal and pectoral4
in the initial stages4
ochraceous and less rufous4
ancestral stock of the4
united at their mid4
is well developed and4
gave rise to the4
in the evolution of4
geomys bursarius majusculus swenk4
desert range experiment station4
referable to the subgenus4
anterior and posterior lophs4
from topotypes of t4
the phyletic development of4
collected by vernon bailey4
incisors longer and wider4
posterior surface of the4
the curtis ranch local4
alveolus of incisor to4
living species of the4
of the uinta mountains4
posterior to nasals short4
hall and bernardo villa4
route from the mississippi4
the cudahy local fauna4
of the lateral re4
and near topotypes of4
in the northern part4
of thomomys bottae wahwahensis4
the southern end of4
bottae occurring in utah4
the patterns of wear4
weaker and less angular4
border of the tooth4
plate on the anterior4
talpoides occurring in utah4
butler springs local fauna4
the fossil record of4
surveys for a railroad4
on the anterior face4
of the colorado piedmont4
interpterygoid space widely v4
the saunders local fauna4
to a high degree4
hay springs local fauna4
the southern rocky mountain4
feet and distal part4
incisors longer and narrower4
of nasals forming a4
d e f g4
in the mountains of4
other members of the4
type and an adult4
the alveolus of the4
of this genus are4
the range of the4
a b c d4
as opposed to v4
of the upper molars4
from topotypes of c4
on the mammals of4
of the lower miocene4
medium in size and4
found to the southeast4
posterior to nasals longer4
san pitch river valley4
history of the university4
of the more specialized4
generalized type of skull4
not so widely spreading4
as opposed to brown4
by pocket gophers that4
modern pocket gophers of4
the upper incisor is4
a vestige of the4
northern limits of its4
in final stages of4
upper parts and sides4
seems to be the4
to the living species4
the type and an4
geographic variation in the4
raymond hall and bernardo4
from it as follows4
of the molariform teeth4
thomomys bottae howelli goldman4
specimens from the type4
as far south as4
distance from alveolus of4
south side of the4
in the western united4
relative to length of4
pliocene and early pleistocene4
of the colorado river4
f g h i4
local fauna of nebraska4
on the posterior surface4
in relation to length4
as far as known4
processes of maxillae heavy4
and colorado by e4
of the third upper4
and surveys for a4
to the latter race4
of the genus cratogeomys4
one side of the4
is inhabited by pocket4
and the posterior plate4
of the two genera4
b c d e4
the long axis of4
e f g h4
the great salt lake4
the virgin river valley4
limits of its range4
as a synonym of4
river to the pacific4
from wyoming and colorado4
w horse creek p4
of the mandible is4
zygomatic arches shorter and4
specimens of this subspecies4
from the mississippi river4
account of that subspecies4
of the range of4
grayish as opposed to4
is of approximately the4
side of the virgin4
the geographic distribution of4
of kansas museum of4
as high as feet4
nose and cheeks dusky4
shape of the zygomatic4
of pocket gophers of4
buff as opposed to4
and not widely spreading4
shorter and more nearly4
kansas state board agric4
of the lower molars4
the remainder of the4
san josecito cave local4
adult females of thomomys4
the basitemporal fossa is4
for the first time4
the first stages of4
in the subgenus orthogeomys4
g h i j4
smaller and less inflated4
loss of enamel plates4
university of kansas museum4
of nasals truncate or4
in the pocket gopher4
eight miles west of4
action of the teeth4
margins of nasals forming4
of the john day4
distinguished from all other4
of the angular process4
shaped rather than lyre4
the sierra del tigre4
restricted to the lingual4
of the subfamily entoptychinae4
by union of the4
range here ascribed to4
the two sides of4
in the early pliocene4
pocket gophers of kansas4
of the early pleistocene4
from the great plains4
josecito cave local fauna4
h i j k4
two sides of the4
the south side of4
oligocene and early miocene4
are separated by a4
a railroad route from4
east of the colorado4
part of the skull4
of the modern genera4
in the ancestral lineage4
the upper cheek teeth4
zygomatic arches weak and4
the animals from the4
size of tympanic bullae4
feet and distal half4
both the anterior and4
valley to the west4
pocket gophers of this4
mississippi river to the4
buffy and less whitish4
differs in smaller size4
an enamel plate on4
thickening at union of4
but to differ as4
of the western mainland4
of pleistocene lake bonneville4
list of kansas mammals4
brown on upper parts4
in size and color4
on the occlusal surfaces4
dorsal profile of skull4
the angular process of3
the center of the3
and not so widely3
of north america and3
of the same species3
easily distinguished from those3
reach the base of3
in addition to the3
the occlusal surfaces of3
raymond hall university of3
and unless otherwise indicated3
nasals actually and relatively3
in upper teeth and3
of each of the3
as in m and3
merriami of the castanops3
number of individuals averaged3
the remains of geomys3
as feet and as3
combined lengths of m3
premolars and third molars3
truncate or shallowly emarginate3
greatest distance across the3
every measurement taken except3
angle of the orbit3
mandible is well developed3
the ecotone between the3
and widest posteriorly rather3
the apex of the3
and wasatchensis see accounts3
darker than topotypes of3
of thomomys bottae trumbullensis3
kinds of pocket gophers3
from the south side3
of utah by stephen3
more widely spreading posteriorly3
pectoral and inguinal regions3
is to be expected3
in the first stages3
plate in the upper3
and an adult female3
most primitive of the3
elongation of the posterior3
is indistinguishable in color3
north america and its3
for comparisons with t3
as opposed to large3
posterior plate in the3
of the bottae group3
the genus geomys from3
subspecies of the species3
of posterior margin of3
from eight miles west3
breadth of rostrum column3
the name thomomys talpoides3
tympanic bullae smaller and3
for the most part3
the two columns at3
in size of the3
upper parts and underparts3
the deep river formation3
on the upper incisor3
tympanic bullae markedly smaller3
of the early and3
longer and more pointed3
in the lower molars3
the tympanic bullae are3
lateral plates of m3
enamel plates on both3
in all of the3
lists of specimens examined3
parts of the state3
accounts of those subspecies3
cinnamon and sayal brown3
to have been deposited3
terms are of ridgway3
species have been described3
of thomomys bottae tivius3
in all parts measured3
has an enamel plate3
grading over sides to3
from cratogeomys castanops subsimus3
the western part of3
early and middle pliocene3
at one end of3
zygomatic processes of the3
the genera orthogeomys and3
grading over the sides3
on the posterior face3
as a subspecies of3
living species of geomys3
wolf creek local fauna3
of these pocket gophers3
of a young individual3
the loan of specimens3
pleistocene records of thomomys3
across the posterior wall3
males and in females3
shown within equal signs3
in relation to the3
fossil record of the3
as opposed to cinnamon3
compare favorably with topotypes3
and that it is3
in response to the3
to the long axis3
on the labial side3
from lake la jara3
suture medially concave or3
the north and east3
as opposed to roughly3
first phases of wear3
in pocket gophers of3
members of the tribe3
of the ancestral stock3
subspecies of geomys bursarius3
rostrum shorter and more3
the size of the3
dorsal surface of the3
in the lower dentition3
is shown by specimens3
uniting at edge of3
the northern limits of3
of anterior and posterior3
with descriptions of new3
the eastern united states3
heavier and more angular3
of the pleistocene lake3
and uninterrupted in all3
from cratogeomys castanops bullatus3
patches small and grayish3
smaller in all measurements3
at the base of3
bullae smaller and less3
small and grayish black3
in other members of3
to the subgenera of3
surface of their protomeres3
processes of premaxillae narrower3
clearest on inguinal and3
fauna is considered to3
been recovered also from3
hall university of kansas3
between cinnamon and sayal3
to be of approximately3
patterns of wear on3
the species thomomys talpoides3
lacrimal processes larger and3
of the tribe dikkomyini3
on the anterior and3
posterior plate of the3
than topotypes of albicaudatus3
is shown within equal3
talpoides from late pleistocene3
with the subspecies of3
the posterior plate in3
chronologic and geographic range3
side of the skull3
both of the lateral3
as opposed to near3
the third lower molar3
the north and west3
fossil lake local fauna3
raymond hall and walter3
early pliocene to recent3
maxillary teeth relatively large3
length of the nasals3
a new spiny pocket3
only a few miles3
on the side of3
is the least specialized3
bullae actually as well3
margin of the tooth3
of stages of wear3
the fossil lake local3
has not been found3
in charge of the3
cent of the individuals3
shape of the nasals3
the doby springs local3
brown as opposed to3
essentially the same as3
of hind foot column3
arches not widely spreading3
a new species of3
are more as in3
of thomomys talpoides moorei3
to lingual end of3
the close of the3
otherwise indicated in the3
the stages of wear3
the subfamily geomyinae by3
the thomomyini and geomyini3
the species of the3
beginning at the northwestern3
the genus thomomys from3
patches medium in size3
in the entoptychines of3
account of that form3
southern end of the3
from the cudahy local3
ends of nasals rounded3
have been recovered from3
posterior face of m3
first stages of wear3
kansas state teachers college3
of dikkomys and pliosaccomys3
the colorado piedmont and3
and lingual side in3
biological surveys collection of3
the lower jaw is3
in the southeastern united3
exceeds the breadth across3
utah by stephen d3
part of the late3
the valleys of the3
can be easily distinguished3
be of approximately the3
size and shape of3
referred species and subspecies3
and zygomatic processes of3
of thomomys talpoides occurring3
part of its range3
of the oquirrh mountains3
the late kansan glaciation3
differs from it as3
of the modern pocket3
of the bicolumnar pattern3
all of the cheek3
space enclosed within zygomatic3
of the skull of3
considered to have been3
two new pocket gophers3
of rancholabrean provincial age3
than combined lengths of3
zygomatic process of squamosal3
part of the great3
a single elliptical column3
structural changes in the3
the subspecies of c3
more widely spreading and3
by tracts of dentine3
in the first two3
the primitive morphotype of3
of wear and the3
averaging no more than3
and postauricular patches grayish3
to the subgenus thomomys3
side of the loph3
range of this subspecies3
of the lower jaw3
in the following features3
alveolar level of mandibular3
for the subfamily geomyinae3
the anterior surface and3
are considered to be3
dentition smaller and weaker3
average and extreme measurements3
of the living species3
from miles west of3
of the genera geomys3
a new subspecies from3
from topotypes and near3
to lambdoidal suture markedly3
the recent mammals of3
is shown within underscores3
in the account of3
in size and black3
in the accounts of3
base of the angular3
is bisulcate as in3
incisors and maxillary teeth3
one or both plates3
the anterior enamel plate3
of the sierra madre3
of the first upper3
in the colorado plateau3
from smiths valley local3
in the collection of3
than any of the3
the same as in3
capitalized terms are of3
the west and south3
processes of maxillae greater3
the western mainland of3
considered to be a3
the entoptychines of the3
thomomys talpoides from late3
of the great salt3
the desert range experiment3
the sierra madre oriental3
found at higher elevations3
west side of the3
pliosaccomys and the geomyini3
sides of the river3
from the posterior wall3
of the occlusal surface3
postauricular patches medium in3
in comparison with t3
western part of the3
along median line of3
section of the great3
processes larger and projecting3
the greatest distance across3
new spiny pocket mouse3
of the type specimen3
of the river are3
opposed to cinnamon buff3
relatively more widely spreading3
anterior and posterior plates3
margin of mesopterygoid fossa3
of the family geomyidae3
arches weak and not3
but differs from it3
of wear in pliosaccomys3
tongues of premaxillae long3
in the area today3
hind feet and approximately3
heavier and more widely3
from upper mississippi valley3
of the late miocene3
been reported from the3
indistinguishable in color from3
found only in the3
the greatest amount of3
underparts pale pinkish buff3
view of lower jaw3
averaging larger in all3
the type specimen of3
are intergrades between moorei3
the late pliocene species3
reduced to lingual side3
the mandible is well3
middle and late pleistocene3
antonio de las alazanas3
side of the river3
the newly erupted tooth3
doby springs local fauna3
the berends local fauna3
entire surface of their3
thomomys bottae absonus as3
border of nasals v3
from the saunders local3
ends of nasals more3
of the species thomomys3
the western and southern3
angular process of the3
list of north american3
the genera geomys and3
shown by specimens from3
to pinkish buff on3
found to the southwest3
occurring in utah by3
creek local fauna of3
length of tail column3
monographic revision of the3
in color and cranial3
comparisons under those forms3
at right angles to3
and alveolar length of3
bullae and tympanic bullae3
the sides of each3
from west to east3
the range of this3
nasals forming a v3
and approximately distal half3
edge of the plains3
the benson local fauna3
bases of hairs plumbeous3
are referred to the3
western united states and3
nasals truncate or shallowly3
is considered to have3
local fauna is considered3
has been recovered also3
specimens are in the3
ends of nasals emarginate3
pattern in the final3
differs in larger size3
in the southern part3
be easily distinguished from3
basilar length of skull3
of first and second3
well developed and massive3
of enamel from the3
the zygomatic arches are3
lingual side in lower3
in the fossil record3
pocket gophers were found3
views of the skull3
primitive morphotype of the3
of the zygomatic arch3
san antonio de las3
sangre de cristo and3
crowns of cheek teeth3
and cheeks grayish black3
three views of the3
postauricular patches large and3
recent mammals of idaho3
russell university of kansas3
readily distinguished from those3
heavy and widely spreading3
straight as opposed to3
gophers of the species3
the great plains province3
the geomyids and heteromyids3
of the masseteric ridge3
on m and m3
subspeciation in pocket gophers3
occlusal surfaces of the3
differ from topotypes and3
upper molar series shorter3
two columns of the3
the time of the3
but more inflated ventrally3
characters are more as3
of dentine on the3
and postauricular patches black3
row a b c3
on the west side3
of the temporal muscles3
in males and in3
between moorei and wasatchensis3
skull of the type3
bullae slightly more inflated3
evolution of the subgenus3
from thomomys talpoides clusius3
and posterior lophs of3
crowns of medium height3
the entire surface of3
ends of nasals truncate3
buffy and less rufous3
anteromedial angle of the3
of the alveolus of3
the collection of the3
the early evolution of3
base of the crown3
to the type locality3
bottae absonus as follows3
amount of geographic variation3
than in other subgenera3
weak and not widely3
genus geomys from the3
from the sequence of3
from the kansas university3
upper and lower premolars3
list of mammals collected3
not as widely spreading3
of the two lineages3
of the rexroad local3
extend the known range3
and hind foot longer3
east of the river3
intermediate between those of3
no gold on underparts3
differ from near topotypes3
mastoid bullae and tympanic3
upper molar series which3
and second upper molars3
zygomatic arches not widely3
any of the other3
are intermediate in color3
northwestern corner of the3
of the posterior part3
edge of the protomeres3
first and second upper3
in the sequence of3
widest posteriorly rather than3
frontomaxillary suture medially concave3
oligocene to middle pliocene3
in the upper dentition3
as in the modern3
at the time of3
classification of the pocket3
in the valleys of3
miles west of rosalia3
and maxillary teeth smaller3
by nelson and goldman3
incisors shorter and wider3
to the south and3
in females compared with3
from alveolus of incisor3
bold text is shown3
has closer affinities with3
lacking a median spicule3
the most highly specialized3
be distinguished from all3
in view of the3
ventral view of lower3
the characters that distinguish3
on both anterior and3
dorsal view of skull3
west of these mountains3
wider and more depressed3
genera orthogeomys and pappogeomys3
anterior margin of mesopterygoid3
tracts of dentine on3
in the present account3
zygomatic arches nearly parallel3
length of nasals column3
gophers of this genus3
three specimens from the3
pleistocene mammals of the3
zygomatic arches widely spreading3
thought to have evolved3
approximately distal half of3
surface of the tooth3
hall and walter w3
nasals and rostrum longer3
of thomomys bottae in3
distribution of thomomys bottae3
as opposed to emarginate3
deer park local fauna3
smaller and slenderer skull3
intergrades between moorei and3
fore and hind feet3
the first phases of3
are less specialized than3
of the modern lineages3
any one of the3
mastoid processes of squamosals3
the ancestral stock of3
the hay springs local3
tympanic bullae actually as3
without trace of enamel3
and otis basin local3
the mammals of the3
entrant folds as in3
enamel from the posterior3
in the development of3
unless otherwise indicated in3
sand draw local fauna3
ancestor of the geomyini3
as opposed to convex3
surface of the skull3
members of the subfamily3
of the wasatch mountains3
the irvingtonian provincial age3
pocket gopher of the3
as opposed to ridged3
of the species geomys3
and loss of enamel3
the east side of3
and a new spiny3
and extreme measurements of3
m and m that3
loss of the posterior3
restricted to lingual end3
key to the subgenera3
enclosed within zygomatic arches3
relation to length of3
in both upper and3
posterior enamel plate on3
posterior to the nasals3
wider posteriorly than anteriorly3
from cratogeomys castanops convexus3
configuration of the skull3
general configuration of the3
the genera of the3
by the following features3
upper parts pinkish buff3
the posterior plate of3
of middle pleistocene age3
of the two lophs3
in the course of3
with the exception of3
more nearly parallel and3
see comparisons under those3
of the southern rocky3
the first upper molar3
in the upper and3
grooving on the upper3
of the modern geomyines3
vertical depth of the3
buff as contrasted with3
in the same sequence3
is reduced to a3
axis of the skull3
well as relatively wider3
upper parts sayal brown3
feet and approximately distal3
raton section of the3
the enamel investment of3
to the posterior surface3
larger in all parts3
of the mammals of3
across the entire surface3
each of the two3
premaxillae posterior to the3
zygomatic arches more robust3
late pleistocene and recent3
upper parts vary from3
potomacensis gidley and gazin3
wasatchensis see accounts of3
on front feet long3
union at the edge3
zygomatic arches more rounded3
on the upper parts3
the development of the3
springs local fauna in3
referable to the latter3
and virgineus in one3
of the two subspecies3
genera geomys and thomomys2
four genera and a2
the ancestor of the2
the entoptychines were the2
is highly specialized for2
the earliest pleistocene records2
lateral expansion of the2
than distance from alveolus2
observations on the rodentia2
thinly overlaid with buffy2
upper reaches of the2
the more specialized genera2
of thomomys bottae occur2
of palate column h2
and short grass zones2
body large for species2
in the main lineage2
assigned to this subspecies2
instead of in females2
and curtis ranch local2
the vertical depth of2
well developed and deep2
is the smallest of2
rostrum wider and longer2
level of mandibular tooth2
the arrangement proposed by2
much larger and more2
investment complete and uninterrupted2
in the valley of2
than twice as long2
colorado and green rivers2
mesopterygoid fossa extending to2
end of the deep2
early evolution of the2
gracilis is of approximately2
completely across posterior wall2
of the supergeneric groups2
body form remarkably fossorial2
to the east of2
species of geomys from2
its structure is essentially2
howard ranch local fauna2
inner border of the2
definitely referable to albicaudatus2
rexroad local fauna referred2
deposits of southwestern kansas2
process of ramus mostly2
history museum of san2
type from benson local2
nasals straight as opposed2
occupy the colorado plateau2
zygomatic arches wider and2
of individuals averaged or2
subspecific status to this2
are found at higher2
primitive in the geomyini2
of the modern species2
margin of the alveolus2
to middle of lateral2
molariform teeth relatively large2
whitish instead of brownish2
referred them to the2
gophers from wyoming and2
having crowns of medium2
planifrons nelson and goldman2
the mountains of central2
the name geomys bursarius2
morrill and garden counties2
used the name thomomys2
lip of upper incisor2
in eastern millard county2
is not known from2
on the one hand2
than in topotypes of2
process of maxilla not2
with description of a2
on all of the2
temporal muscles remaining separated2
larger size throughout and2
the reduction of enamel2
pigmented as opposed to2
listed in roman type2
and elliptical in cross2
the two lophs of2
dentine on the sides2
and convexus by larger2
of the crown to2
of thomomys talpoides oquirrhensis2
cratogeomys castanops rubellus nelson2
among named subspecies of2
smaller and more nearly2
pattern characteristic of the2
surface of the posterior2
lisco local fauna of2
localities in colorado may2
the specimens of thomomys2
down the virgin river2
front feet long and2
subfamily geomyinae by robert2
majusculus differs in larger2
jugals more nearly straight2
top of head and2
in shape of the2
geomys quinni from the2
hind foot and tail2
county are not typical2
surface of the newly2
the mammals of colorado2
local fauna of meade2
color and cranial features2
a dark dorsal stripe2
south of spanish fork2
on sides and flanks2
and wider posteriorly than2
premaxilla posterior to nasals2
lake city and environs2
is the smallest subspecies2
intergradation between lenis and2
became adapted to the2
are retained in the2
few miles to the2
fauna from meade county2
color terms are those2
the upper reaches of2
progressive loss of the2
castanops planifrons nelson and2
loss of the bicolumnar2
the late pleistocene and2
between robustus and albicaudatus2
tivius and stansburyi are2
region of north america2
subspecies to the southward2
ranges of these two2
smaller species of geomys2
and nonangular as opposed2
reference is made to2
in the colorado river2
length of upper molariform2
p at alveolar border2
those in charge of2
is less specialized than2
the material at hand2
the alveoli of the2
of the ancestral lineage2
from the fox canyon2
from the ancestral stock2
z m rb i2
this is especially true2
rise to the modern2
enamel pattern of the2
evolution of the modern2
is currently regarded as2
lips of molariform teeth2
the platycephalic skull is2
of in females and2
interpterygoid space moderately v2
subspecies of thomomys umbrinus2
in the western part2
assigned to the genus2
thomomys talpoides oquirrhensis as2
configuration of the first2
the m and m2
cheeks and postauricular patches2
cinnamon buff as opposed2
posterior end of nasals2
from the dixon are2
of thomomys bottae virgineus2
from the early miocene2
is one of the2
projecting higher above anteromedial2
e slope mount ellen2
over sides to pale2
thomomys perpallidus centralis hall2
a synonym of the2
sandhills on birdwood creek2
that the pattern of2
enamel blade on the2
molar series which are2
kansas and its climatic2
into the late pleistocene2
as in the living2
to be referable to2
in part supporting cheek2
from thomomys bottae albicaudatus2
males and females of2
one of the more2
the early pleistocene and2
zygomatic arches more nearly2
of p at alveolar2
cratogeomys castanops sordidulus is2
the pleistocene of the2
form of third upper2
rufous and less buffy2
third of anterior surface2
middorsal depression in frontals2
thomomys bottae levidensis goldman2
as it does in2
first and second lower2
of the arkansas river2
are of approximately the2
the skull is generalized2
josecito cave in nuevo2
in the curtis ranch2
enamel plate of m2
interesting to note that2
referred to the species2
zygomatic arches markedly less2
side of upper tooth2
m rb i a2
on the distribution map2
of the cranial details2
of the foramen magnum2
in of specimens of2
entoptychines of the early2
and two lateral plates2
in nearly every measurement2
mainland of the pleistocene2
flora of the tertiary2
resembling that of g2
de cristo and wet2
a list of kansas2
represent parts of lineages2
the same in the2
seems to be a2
to of zygomatic breadth2
been deposited in late2
on the enamel cap2
with thomomys bottae aureiventris2
of the larger subspecies2
zygogeomys have been found2
of m reduced to2
part of the valley2
thomomys bottae convexus durrant2
pocket gophers and their2
the insertion of the2
pocket gophers as a2
thomomys is unknown from2
at the northwestern corner2
always wider than long2
of cerro viejo de2
bonnevillei differs as follows2
was equivalent to the2
the northern boundary of2
of the posterior surface2
in region of interparietal2
along the dorsal border2
grading through cinnamon on2
of the rostrum and2
lineage of the thomomyini2
the subfamily entoptychinae are2
berends local fauna in2
molariform teeth markedly smaller2
have not been identified2
slightly darker brown on2
the generalized type of2
by being smaller in2
contractus differ from those2
formations of the west2
but little from dikkomys2
a junior synonym of2
referred twelve specimens from2
and second molars in2
with greatest width posteriorly2
by the lack of2
one or both lateral2
to anterior border of2
are intergrades between centralis2
intergradation of the two2
subspecies is the smallest2
of the lower molariform2
the beginning of this2
certainly to scott county2
in the phyletic development2
the snake river drainage2
subgenera pappogeomys and cratogeomys2
braincase more nearly flat2
be distinguished from the2
instead of in males2
the loss of the2
the field museum of2
the north platte river2
upper pleistocene records of2
indistinguishable in color and2
and forms a conspicuous2
alveolus of first upper2
lower molars and the2
less widely spreading posteriorly2
except for a slight2
of the molariform dentition2
the race to the2
shorter and more recurved2
queen of sheba canyon2
and second lower molars2
the history of the2
from as low as2
which are intergrades between2
the butler springs local2
talpoides oquirrhensis as follows2
of wear as the2
enlargement of the masseteric2
of stansbury island that2
the range of t2
surveys collection of the2
enamel plates of m2
the lateral plates on2
with thomomys bottae planirostris2
the enamel blade on2
the geomyinae and the2
to be more closely2
nasals actually as well2
incisor to anterior border2
differ from the topotypes2
accounts of the subspecies2
anterior plate in the2
the university of michigan2
and relatively more widely2
and tobin local faunas2
specimens in question are2
pocket gophers were taken2
forms a conspicuous heel2
local fauna in meade2
specimens of thomomys bottae2
to nearly white on2
mountains south of spanish2
modern pocket gophers and2
breadth across the zygomatic2
and as high as2
key to the genera2
from thomomys talpoides macrotis2
i a e s2
to the south in2
like planirostris in four2
in fresh winter pelage2
sevier river valley from2
states biological surveys collection2
across posterior wall of2
from benson local fauna2
anteroposterior compression of the2
and posterior wall of2
with thomomys bottae lenis2
most closely resemble those2
new pocket gopher of2
is noted in the2
between ocius and uinta2
as opposed to rounded2
explorations and surveys for2
of this species inhabit2
topotypes of contractus differ2
pine valley to the2
sought for elsewhere on2
of the basitemporal fossa2
upper parts in winter2
with light brown hairs2
zygomatic arch broadly and2
at elevations as low2
subspecies to the west2
thomomys talpoides oquirrhensis durrant2
same as in the2
cratogeomys castanops subnubilus nelson2
the colorado piedmont is2
a synopsis of the2
center of differentiation for2
geomys from the rexroad2
incisor to middle of2
are in the university2
in an intermediate stage2
outer and inner re2
a result of the2
specimens of each sex2
plate is retained in2
upper parts mummy brown2
mainland of pleistocene lake2
the dorsal surface of2
castanops excelsus nelson and2
as is indicated by2
or both of the2
figure in text august2
tertiary formations of the2
a e s rl2
the bicolumnar crowns of2
is laid top down2
the anterior palatine foramina2
geographic range of t2
of the rostrum relative2
twice as long as2
angular process of mandible2
is the most specialized2
new pocket gopher from2
alveolus of the first2
small and deeply pigmented2
were taken at elevations2
in advanced stages of2
clear creek camp of2
the first time in2
pinkish buff as opposed2
races of thomomys talpoides2
the specimens from kansas2
hairs of feet whitish2
to that of the2
species the posterior loph2
of rostrum column i2
the zygomatic processes of2
pleistocene vertebrates from the2
the fox canyon locality2
topotypes of wasatchensis can2
the distance from the2
faunal lists of the2
of north american recent2
have been published in2
two columns united at2
united states forest service2
is arranged as a2
bullae much larger and2
of geomys and pappogeomys2
form to the east2
a number of species2
pleistocene lineages of the2
geomyini in the late2
from the miocene of2
the lingual edge of2
america and its vertebrated2
the pocket gophers are2
wahwahensis show them to2
the relative abundance of2
planirostris and birdseyei in2
county from north to2
and tympanic bullae more2
the eastern and western2
in topotypes of albicaudatus2
fossa receives the insertion2
averaging not more than2
the west of these2
premolar and first two2
ravus differs as follows2
of the main line2
primitive character of the2
the primitive bicolumnar pattern2
reduction of enamel in2
extensive ranges of any2
darker on upper parts2
of a single species2
geomys hispidus le conte2
the affinities of the2
distinguished from thomomys bottae2
than being strongly recurved2
having two columns joined2
pure white to roots2
of the five subspecies2
madre mountain range of2
see account of phylogeny2
retract the lower jaws2
sagittal crest in adult2
to pale pinkish buff2
abruptly narrow at one2
late oligocene and early2
the most extensive ranges2
drawings illustrating enamel patterns2
opposed to large and2
process of the mandible2
posterior to nasals s2
strongly recurved upper incisors2
averaging in females compared2
prismatic character of molars2
m has not been2
masseteric ridge on the2
across the mastoid processes2
low as feet and2
early stages of wear2
on the north by2
at region of maxillo2
of geomys and thomomys2
vertical when skull is2
west slope sierra de2
local fauna referred to2
pale pinkish buff on2
have essentially the same2
zygomatic breadth column g2
in pappogeomys bulleri and2
from cratogeomys castanops excelsus2
and birdseyei in two2
john simon guggenheim memorial2
those from the mountains2
camp of minnedoka national2
most closely related to2
cumberland cave local fauna2
geomys lutescens jugossicularis hooper2
in the snake river2
with a median ventral2
approximately the same color2
convex rather than flat2
of the two grooves2
posteriorly rather than anteriorly2
the enamel bands are2
not inhabited by pocket2
upper molar series long2
gopher remains from the2
the eastern side of2
central part of the2
geomys bursarius has been2
the one hand and2
length of nasals and2
found in the curtis2
locality of the rexroad2
the two prisms are2
the colorado river drainage2
nasals rounded posteriorly as2
to be the most2
parts between cinnamon and2
distance across the zygomatic2
the other of the2
lineages of the geomyini2
pocket gopher from the2
may be correlated with2
with the result that2
posterior face of the2
by animals belonging to2
nose and cheeks grayish2
field notes by the2
ben franklin local fauna2
united across the entire2
pointed and with more2
cratogeomys pappogeomys tylorhinus from2
late pliocene and pleistocene2
and having crowns of2
did not develop in2
are lighter in color2
as a valid species2
is evident in the2
intergrade between planirostris and2
the primitive characters of2
mouth of reddicks canyon2
illustrating enamel patterns characteristic2
a high degree of2
the north end of2
of these animals are2
between planirostris and trumbullensis2
the known species of2
a trait that is2
to the lingual side2
thomomys bottae centralis hall2
of the known genera2
the medicine bow mountains2
the specific characters are2
the inner side of2
enamel plates from the2
other genera of the2
show some intergradation with2
hind foot column e2
posterior to nasals shorter2
from the middle pleistocene2
reduction of the posterior2
junior synonym of zygogeomys2
trends in subfamily geomyinae2
side in upper molars2
the color and size2
individuals averaged or catalogue2
planirostris to which they2
see accounts of the2
inferior border of premaxillary2
type from fossil lake2
and posterior tongues of2
w foot pico de2
actually and relatively longer2
full species of the2
have been deposited in2
two lophs of the2
two columns joined at2
is retained throughout life2
evolved in response to2
rows of the tribe2
one of the modern2
the dirty devil river2
may be characterized as2
of each upper incisor2
the patterns of m2
the ancestral tribe dikkomyini2
flattening of the skull2
to the atlantic coast2
column in the final2
with field notes by2
of the lower pleistocene2
natural history museum of2
the rostrum relative to2
of a new subspecies2
first time in this2
united states in the2
these fossils may be2
and the occlusal surface2
specimens from mcpherson county2
the mountains and high2
in colorado by phillip2
the taxonomic status of2
characteristic of the living2
pappogeomys the genus pappogeomys2
planirostris from zion national2
terms are those of2
from the two sides2
mountains in the southern2
buff on the underparts2
depth of skull rl2
the upper parts and2
from the saw rock2
is interesting to note2
to level of posterior2
an early stage of2
the labial side and2
of maxillary tooth row2
springs local fauna of2
in his description of2
weak and nonangular as2
narrower and more recurved2
from the posterior face2
posterior wall of tooth2
series which are larger2
pleistocene of north america2
named subspecies of thomomys2
zygomatic arches more angular2
n l t h2
industrius differs from g2
arched rather than straight2
thomomys bottae tivius by2
stages of attrition in2
of the field museum2
is essentially the same2
the sierra nevada de2
rufous and less pinkish2
at the type locality2
the occlusal pattern of2
is remarkably stable in2
in the pattern of2
of maxillae weaker and2
front feet and hind2
ridged and more nearly2
united states biological surveys2
of the genus is2
of the pocket gopher2
higher above anteromedial angle2
teeth markedly smaller and2
in table on this2
wider across zygomatic arches2
with most of the2
kane and garfield counties2
of thomomys talpoides in2
primitive characters of the2
majority of characters are2
on the two sides2
pocket gophers that belong2
pliocene and middle pleistocene2
extreme measurements of five2
southwestern united states in2
length of rostrum n2
specialized trends in the2
of premaxilla posterior to2
one enamel plate on2
the animals from st2
level of jugal bone2
thomomys bottae aureiventris as2
of incisor to anterior2
the angular process is2
females and instead of2
from type locality male2
of cratogeomys castanops angusticeps2
higher elevations to the2
with planirostris from zion2
the hamulus of the2
is only slightly darker2
the most closely related2
a single column in2
longer in relation to2
no larger than the2
beds along the north2
as opposed to lyre2
are separated by an2
sierra madre mountain range2
of kansas by bernardo2
convexus nelson and goldman2
nearly every measurement taken2
the wasatch mountains south2
anterior plates of lower2
b na z m2
length of tail h2
in the western and2
labial side of the2
the skulls are more2
spinous process at jugal2
are too fragmentary to2
remains of thomomys umbrinus2
the cudahy and tobin2
the elongation of the2
and posterior columns at2
anterior palatine foramina are2
parts and sides lighter2
a stage in the2
attrition on the occlusal2
at the present time2
sw slope bald peak2
after the glacial maximum2
elevations from as low2
until the early pliocene2
genera of pocket gophers2
or catalogue number l2
vestige of the primitive2
l t h b2
masseteric ridge weakly developed2
ranges of the two2
from eastern colorado by2
the genus geomys in2
lutescens in kansas is2
the pleistocene of north2
would have produced the2
enamel plates are complete2
emarginate posteriorly as opposed2
between it and centralis2
prove these animals to2
of a single elliptical2
from the medicine bow2
to lingual side or2
is evident on the2
half of tail whitish2
differs in slightly darker2
front feet longer and2
intergrades between robustus and2
but always wider than2
less specialized than the2
enamel plate of posterior2
of the early evolution2
averaging instead of in2
less ridged and angular2
the pattern characteristic of2
howelli occupy the colorado2
lateral border of p2
earlier stages of wear2
of maxillae much heavier2
is especially noticeable in2
unite at the edge2
are listed by counties2
lophs are separated by2
more pointed and with2
the position of the2
impressions of temporal muscles2
t h b na2
a small pocket gopher2
on front feet small2
is found in the2
of three adult females2
by counties from west2
plate restricted to the2
lambdoidal crests perpendicular to2
of the genus pappogeomys2
bullae less inflated ventrally2
on the north side2
maxillary teeth relatively larger2
tail and end of2
maxillary arm of the2
east of the sangre2
from the fossil lake2
are indistinguishable in color2
united states until the2
lingual end of the2
in the size and2
of late pliocene age2
the premolars and third2
m and m would2
the teeth of the2
this area is an2
and named as follows2
geomys bursarius jugossicularis hooper2
of the deep creek2
may be known as2
from left to right2
at elevations from as2
in size of body2
resemble uinta in size2
the animals from fairfield2
the final stage in2
the central part of2
the course of my2
angular process of ramus2
on the angular process2
shaped rather than v2
the anteromedial angle of2
crest in adult males2
of southwestern coahuila and2
both p and p2
the account of that2
shape of a u2
processes of premaxillae wider2
upper incisor is bisulcate2
zygomatic arches and tympanic2
the most primitive of2
the cheek teeth of2
acutus differs as follows2
of zygogeomys have been2
the deer park local2
taken at elevations as2
curtis ranch local faunas2
the primitive lineage of2
lingual edge of the2
depth in part supporting2
of the animals are2
nasals shorter and more2
from mile east of2
dorsal surface of skull2
to the family geomyidae2
tracts of dentine that2
in shape as opposed2
an intermediate stage in2
depression in frontals present2
fauna in meade county2
columns at the edge2
new species of pocket2
race nearest geographically to2
ridge is well developed2
geomys from the dixon2
of the age of2
all of the named2
tooth cave local fauna2
maxillary tooth row e2
more of the primitive2
percent of basilar length2
from wisconsin deposits in2
from the east side2
out that the saunders2
supergeneric groups of rodents2
and phrases are marked2
are as in planirostris2
the vicinity of tala2
result of these studies2
the lingual and labial2
the animals of the2
the pattern of grooving2
western and southern parts2
gophers and their immediate2
in a majority of2
dikkomys of the early2
incisors shorter and more2
the skulls are intermediate2
description of stages of2
the aggregate of characters2
for a discussion of2
late pliocene and middle2
upper parts light ochraceous2
the two columns are2
tongues of premaxillae shorter2
words and phrases are2
the green and colorado2
upper molar series longer2
posterior plates of upper2
pronounced vertical depth in2
are referable to moorei2
nearly white on underparts2
borders of the interparietal2
blade on the posterior2
history university of kansas2
from the oquirrh mountains2
half of the tooth2
incisors short and strongly2
plate on the lingual2
the subspecies to follow2
of the upper cheek2
zygomatic plate of maxilla2
in the first and2
darker brown on upper2
of the primitive structure2
darker than rest of2
from fossil lake beds2
wasatchensis differs as follows2
the classification of the2
posterior enamel plate is2
dorsal depression present in2
nearly parallel and not2
merit separation and naming2
angular part of mandible2
the masseteric ridge is2
uninterrupted in all stages2
late pleistocene records are2
in a series of2
thomomys talpoides gracilis durrant2
at higher elevations to2
may extend the known2
thomomys quadratus uinta hall2
equal to distance from2
upper molar series short2
the columns at the2
to impressions of temporal2
reported the genus from2
only in early stages2
this newly described subspecies2
thomomys talpoides levis goldman2
descriptions of new species2
the highest degree of2
less than per cent2
end of the tooth2
of the superfamily geomyoidea2
adults of both sexes2
the premolars and molars2
in any one of2
separated by an intervening2
termed the loup fork2
the age of the2
in northern new mexico2
upper parts between cinnamon2
is known to occur2
extensions of premaxillae long2
dolichocephalic and platycephalic specializations2
the panhandle of texas2
to the genus zygogeomys2
specimens from lake la2
alveolar lip of upper2
are here referred to2
process and the third2
as far north as2
counties from west to2
entrant angles on the2
feet and hind feet2
the national science foundation2
and the third lower2
to this subspecies from2
in all living geomyini2
the early miocene and2
records of thomomys are2
sierra nevada de colima2
w san antonio de2
wahwahensis differs as follows2
more ridged and angular2
medially concave or straight2
it can be distinguished2
of the middle pliocene2
the account of the2
have been reported from2
description of a new2
durrant university of kansas2
be distinguished from thomomys2
of tympanic bullae and2
upper parts snuff brown2
monographs of north american2
is properly to be2
border of p at2
in slightly lighter color2
upper incisors wider and2
in an early stage2
considered to be from2
of third upper molar2
of hind foot b2
of the type locality2
of the upper parts2
anterior extension of the2
well developed in all2
the buis ranch beds2
of lateral border of2
except in one species2
river valley from piute2
foramen magnum larger and2
phyletic trends in subfamily2
referred to the latter2
creek camp of minnedoka2
be distinguished as follows2
the lower molars and2
arches and tympanic bullae2
the maximum of millimeters2
thomomys bottae wahwahensis durrant2
see white and downs2
from lower harrison deposits2
we are grateful to2
than it is to2
collection of the united2
and the occlusal pattern2
and classification of the2
a result of these2
north platte river valley2
greatest length of the2
border of alveolus of2
of the labial re2
reduction and loss of2
the general configuration of2
four new pocket gophers2
considered by him to2
account of the latter2
posterior walls of the2
headings in table on2
between planirostris and birdseyei2
wasatch mountains by the2
anteriorly rather than being2
detailed description of stages2
total length less than2
the area between the2
the subgenus pappogeomys is2
lambdoidal suture markedly less2
mile east of garrison2
wear in the geomyini2
breadth across the mastoid2
the douglas fir zone2
processes of maxillae much2
between the two named2
other subspecies of thomomys2
as would be expected2
of upper tooth and2
from m and m2
the presence of a2
the level of subgenera2
simon guggenheim memorial foundation2
the same sequence of2
colorado by phillip m2
are inhabited by pocket2
surface and another on2
the upper and seven2
interpterygoid space moderately lyre2
of tail column d2
differs in the following2
weaker and less widely2
of the less specialized2
plane of posterior wall2
surfaces of the molars2
and the butler springs2
its range to the2
stages of phyletic development2
ridge is distinct but2
the labial side of2
is set apart in2
referred the same specimens2
the inner border of2
distribution of this subspecies2
of the colorado and2
pocket gophers is uncertain2
allen thomomys aureus allen2
and end of tail2
thomomys bottae internatus goldman2
printed by fred voiland2
in the first phases2
the dentition and the2
the two columns unite2
length of the rostrum2
of these animals and2
outline of dorsal profile2
to the subgenus heterogeomys2
from the sierra nevada2
species of pocket gopher2
patterns based on nos2
was found in the2
thomomys talpoides levis and2
specimens from coventry are2
that the animal from2
the sand draw local2
retained on the lingual2
patches large and black2
the early stages of2
from base of rostrum2
to be of miocene2
intergrades between planirostris and2
dentitions of the tribe2
color slightly darker brown2
decrease in depth of2
rounded posteriorly as opposed2
specializations of the skull2
new mexico and colorado2
across the squamosal processes2
recorded the genus geomys2
gophers were taken at2
length more than mm2
slight attrition on the2
the angular processes are2
they resemble uinta in2
plates of m usually2
this part of the2
character of enamel patterns2
nasals more deeply emarginate2
the deep creek mountains2
deeply pigmented as opposed2
plate in the lower2
length of palate column2
pleistocene deposits of the2
the pocket gophers as2
tube of auditory bulla2
i am grateful to2
in that part of2
to the subgenus pappogeomys2
be more closely allied2
the anterior plate of2
and adjacent parts of2
referred to the subgenus2
the primitive subtriangular pattern2
only a slight inflection2
and raton section of2
from miles east of2
bottae aureiventris as follows2
another on the posterior2
the west of the2
skull medium in size2
from the northern part2
that the animals from2
of the sangre de2
inhabited by animals belonging2
barriers to the passage2
and southern parts of2
is regarded as the2
all referable to albicaudatus2
across posterior walls of2
anterior lophid of lower2
described and named as2
from the rexroad local2
castanops consitus nelson and2
geomys tobinensis from the2
alveolar lips of molariform2
pleistocene mammalian fauna from2
southwestern part of the2
an isolated enamel fossette2
the oquirrh mountains are2
the decrease in depth2
found the remains of2
ancestral lineage of the2
of the birds of2
pocket gophers of utah2
is closely allied to2
of cratogeomys castanops clarkii2
in the molars of2
more like those of2
are elliptical in cross2
ventral surface of tail2
the southern rocky mountains2
found beyond the mountains2
salt lake city and2
animals from the east2
anterior border of alveolus2
color and in cranial2
no longer than wide2
below alveolar level of2
from the conard fissure2
palate and nasals shorter2
the center of differentiation2
the unworn enamel cap2
found within the state2
developed by that time2
to the genus thomomys2
collected by annie m2
and pectoral regions pale2
having four enamel plates2
compared with cratogeomys castanops2
pattern of wear and2
the coronoid process and2
skulls closely resemble those2
colorado plateau province of2
field museum of natural2
frontomaxillary sutures convex medially2
having one enamel plate2
e horse creek p2
in slightly darker color2
to the genus pappogeomys2
rubellus nelson and goldman2
upper parts buckthorn brown2
plate of posterior wall2
of p restricted to2
and bernardo villa r2
at any stage of2
of the newly erupted2
or exceeds the breadth2
only from the recent2
that part of stansbury2
of the state south2
the range of variation2
side in lower teeth2
magnum larger and more2
end of tail white2
from new mexico and2
than per cent of2
the separation of the2
occurring only in the2
anteroposterior occlusal length of2
the shape of a2
rafinesque mus bursarius shaw2
width across alveolar processes2
length of lingual plate2
from the northern limits2
valley from piute county2
specimens assigned to this2
of mammals collected by2
below the pearlette ash2
the terminal stages of2
castanops rubellus nelson and2
longer than wide owing2
are grateful to dr2
of specimens of rostralis2
quadrangular as opposed to2
to large and lightly2
the palest specimens of2
during the aftonian interglacial2
is more closely allied2
the masseteric ridge on2
larger and more ovoid2
the east and south2
status to this animal2
thomomys talpoides in east2
arches shorter and more2
zygomatic arches heavy and2
planirostris in four measurements2
to which it is2
by him to be2
of parowanensis from the2
abruptly from base of2
length of m and2
be characterized as follows2
cratogeomys castanops planifrons nelson2
inner side of the2
for its effacement would2
the anterior wall of2
one or a few2
of the green river2
arm of the zygomata2
edge of the tooth2
extending to level of2
the bicolumnar pattern in2
thomomys talpoides uinta goldman2
characteristic of the modern2
the superficial masseter muscle2
nearly parallel and less2
with thomomys bottae stansburyi2
crests perpendicular to sagittal2
san josecito cave in2