「Devonian」の共起表現一覧(1語右で並び替え)
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The origins of the name Brentor are old | Devonian, a Brythonic Celtic language related to Corni |
It was among the most basal of the | Devonian actinopterygians and is considered the first |
Most of the valley is cut into | Devonian age shale, sandstone, and limestone. |
impson Formation is a stratigraphical unit of | Devonian age in the Western Canadian Sedimentary Basin |
fossil site is a paleontological site of late | Devonian age in the central west of New South Wales, A |
prises mainly a series of limestones of early | Devonian age and is one of the most fossiliferous regi |
are formed from sandstones of Ordovician and | Devonian age together with a suite of both intrusive a |
sion Lycopodiophyta of ?Late Silurian to Late | Devonian age (around 420 to 360 million years ago), fo |
Carboniferous age, intruded into surrounding | Devonian age "killas" - a series of metamorphosed sedi |
dstones of the Brownstones Formation, also of | Devonian age, which form the bulk of the hill. |
ves of late Silurian or (more commonly) Early | Devonian age, found in Europe, North America, western |
ifically a quartz diorite to granodiorite) of | Devonian age, which has intruded into the gneiss of th |
ifically a quartz diorite to granodiorite) of | Devonian age, which has intruded into the gneiss of th |
lateau Beds Formation which are of upper/late | Devonian age. |
re upfolded amidst Old Red Sandstone rocks of | Devonian age. |
lateau Beds Formation which are of upper/late | Devonian age. |
m greywackes) and limestones of Ordovician to | Devonian age; and |
ition of the killas strata is spread over the | Devonian and Carboniferous geological periods. |
Its rock layers and bedrock are primarily | Devonian and Silurian shale and sandstone. |
ng Ordovician rocks are overlain by disturbed | Devonian and Mississippian rocks. |
oric coelacanth fishes which lived during the | Devonian and Carboniferous period. |
nowledge especially of the vertebrates of the | Devonian and older rocks. |
id extensive research on fossils found in the | Devonian and Silurian geological strata of the Baltic |
Geologically, the area belongs mainly to the | Devonian and Culm formation in which slate, greywacke |
Through the Ordovician, Silurian, | Devonian, and early Carboniferous, marine sedimentatio |
The overlying | Devonian and Carboniferous age sandstones, mudstones a |
o a lesser degree throughout the Silurian and | Devonian, and then again during the Carboniferous. |
urred at dawn the next day, on 4 August, when | Devonian and Cornish forces defending Clyst St Mary ca |
reached a peak in diversity during the Early | Devonian and were found throughout the world, particul |
Numerous | Devonian and Carboniferous plutons are also found. |
There are also strata from the | Devonian, and Mississippian periods. |
formed 250-350 million years ago, during the | Devonian and Silurian periods, when the sands and silt |
Polythecophyton was a genus of Early | Devonian aneurophyte with branching axes, drooping, ma |
His studies with Newberry of the placoderms, | Devonian armored fishes, eventually resulted in Dean's |
le Butterfly formation was found in the upper | Devonian beds of North Cornwall. |
For the botanical garden near Devon, see | Devonian Botanical Garden. |
Early work dealt with | Devonian brachiopods in the Kyrgyzstan portion of the |
me older fossils have been described from the | Devonian, but paleontologists disagree about whether t |
es and of the Basin of Oviedo, Spain; on the ( | Devonian) Calcaire d'Erbray; on the Palaeozoic rocks o |
park are (in ascending stratigraphic order): | Devonian Catskill Formation, the Mississippian-Devonia |
Turnoceras is | Devonian cephalopod belonging to the oncocerid family |
The dam foundations are weathered | Devonian conglomerates, sandstones and shales. |
Asmussia murchisoniana was a | Devonian crustacean of the class Branchiopoda. |
Platyceras is particularly abundant in | Devonian deposits (359 million to 416 million years ol |
Devonian Elementary (3rd Grade) | |
th the rest of the placoderms during the Late | Devonian extinction event. |
tinct ammonoid cephalopod genus from the Late | Devonian, Famennian stage. |
m his personal fossil collection, including a | Devonian fish, a Sauropod vertebrate, and a Trilobite |
sozoic fossils on display, including numerous | Devonian fish. |
ite is important as the youngest locality for | Devonian fossils in New South Wales, containing a dive |
von, and on the Palaeontological Value of the | Devonian Fossils (1867). |
th Africa, the Polar regions, and notably the | Devonian fossils of Germany, Bohemia and other parts o |
oides is an extinct genus of trilobite of the | Devonian found in Morocco. |
urope from the middle Ordovician to the early | Devonian from 472-412.3 mya, existing for approximatel |
Opening in 1977, | Devonian Gardens was designed by J.H. Cook Architects |
Devonian Gardens is a large indoor park and botanical | |
quare part of The Core Shopping Centreand the | Devonian Gardens urban park. |
At 2.5 acres (1.01 ha), the | Devonian Gardens is one of the largest urban indoor ga |
It also contains the | Devonian Gardens, a unique 2.5-acre (1.0 ha) glass-enc |
Grossopterus overathi (Gross, 1933) - | Devonian, Germany |
Its fossils are found from Early | Devonian Germany, ranging from the late Emsian epoch u |
of the order Rhenanida, of the seas of Early | Devonian Germany. |
Acrimeroceras is an oxyconic | Devonian gonitite and one of three genera included in |
n, VIDO was established with funding from the | Devonian Group of Charitable Foundations, the Province |
oid that lived from the Silurian to the Early | Devonian in North America. |
sk that lived from the Silurian to the Middle | Devonian in Africa, Europe, and North America. |
ived from the middle Ordovician to the middle | Devonian, in Africa, Europe, North America, and South |
niatitid ammonoinds from the MIddle and Upper | Devonian included in the suborder Tornoceratina. |
is a class of early vascular plants from the | Devonian, informally called trimerophytes. |
h Cephalaspis was found only during the early | Devonian, it is shown being pursued by the Late Siluri |
Large rugose coral (above hammer) in the | Devonian Jeffersonville Limestone at the Falls of the |
Guangnania was a genus of Early | Devonian land plant with branching axes. |
Sporogonites was a genus of Lower | Devonian land plant with branching axes. |
"A reinterpretation of the Early | Devonian land plant, Bitelaria Istchenko and Istchenko |
he evolution of large land plants in the late | Devonian led to increased organic carbon burial and co |
nurus ("Twin head-tail") was a genus of Lower | Devonian lichid trilobites that lived in a shallow sea |
owever, a significant area of the fossil-rich | Devonian limestone rock is still left exposed, and is |
Devonian limestones were found in Telen River, East Ka | |
along the Sulphur Mountain Thrust Fault below | Devonian limestones. |
ars old, they are usually found as fossils in | Devonian marine rocks. |
vidence for sedimentary-source changes in the | Devonian miogeocline of the southern Canadian Cordille |
Devonian Motor Services | |
he basalt intrudes through the gently dipping | Devonian Needmore Formation (fossiliferous shale and c |
family Nothoceratidae, known from the Middle | Devonian of central Europe and Upper Devonian of Austr |
Asteriacites from the | Devonian of northeastern Ohio; this trace was made by |
t genus of ptyctodont placoderm from the Late | Devonian of Europe. |
extinct petalichthid placoderm from the Early | Devonian of China. |
Gluteus minimus is a fossil from the Upper | Devonian of Iowa. |
t lived in the Late Eifelian epoch (of Middle | Devonian) of Spain. |
spid fish from the Late Silurian to the Early | Devonian of Europe. |
e lycophyte, known as fossils from the Middle | Devonian of Australia, North America, Germany, and Bel |
t genus of ptyctodont placoderm from the Late | Devonian of Germany (Orvig 1960). |
Spyroceras is pseudorthocerid genus from the | Devonian of North America and Europe, defined by Hyatt |
a in Canada, China and Russia, as well as the | Devonian of Germany. |
rotornoceras is a tornoceratid from the Upper | Devonian of Europe with an open umbilcus and sutures t |
Hederelloids encrusting a brachiopod from the | Devonian of Ohio. |
It was found in the | Devonian of New York. |
nt of hydrogen like the eastern United States | Devonian oil shales. |
1982 for processing the eastern United States | Devonian oil shales. |
d slabs of local flagstone that come from the | Devonian Old Red Sandstone. |
trapodomorph fossils are known from the early | Devonian onwards, and include Osteolepis, Panderichthy |
estimated to be less than 400 million years ( | Devonian or earlier). |
Ice Mountain is a large mass of | Devonian Oriskany sandstone and Marcellus shale with n |
ttle "a third British victory at Hehil in the | Devonian peninsula". |
xtinct placoderm fish, which lived during the | Devonian period of North America. |
Gooloogongia lived during the Late | Devonian period (Famennian stage, about 360 million ye |
nus of placoderm fish, which lived during the | Devonian period of Norway. |
This genus is from the | Devonian period and can be found in Morocco. |
an extinct fish which lived during the Early | Devonian period (Late Lochkovian), of south China, Quj |
placoderm fish, which lived during the Middle | Devonian period of North America. |
f placoderm fish, which lived during the Late | Devonian period of Europe. |
nus of placoderm, which lived during the Late | Devonian period of Spitsbergen, Norway. |
f placoderm fish, which lived during the Late | Devonian period of North America. |
ish, about 2 cm, which lived during the Early | Devonian period of China. |
nus of placoderm fish, which lived during the | Devonian period of East Asia. |
placoderm fish, which lived during the Middle | Devonian period of North America. |
ers of sandstone and mudstone dating from the | Devonian period and ascribed to the Lower Old Red Sand |
sandstones and mudstones deposited during the | Devonian period and known collectively as the Old Red |
ehistoric eurypterids that lived in the Lower | Devonian period in Europe and possibly North America. |
independently by several plant groups in the | Devonian period as part of the process of evolution of |
anching, leafless land plants, known from the | Devonian period and first described in 1969. |
lobe-finned fish which lived during the Late | Devonian period (about 374 to 359 million years ago). |
ct genus of ray-finned fish that lived in the | Devonian period of Europe and North America. |
lobe-finned fish which lived during the Late | Devonian period (Frasnian stage, about 375 to 385 mill |
lobe-finned fish which lived during the Early | Devonian period (Pragian stage, about 407 to 411 milli |
cliffs show a timeline of the Middle to Early | Devonian period hundreds of millions of years ago. |
em of north Western Australia during the Late | Devonian period (c. |
f Tristichopterid fish that lived in the Late | Devonian period (Famennian) of Australia. |
of tetrapod-like fish that lived in the Late | Devonian period (Late Givetian to Early Frasnian). |
ago, with volcanic activity occurring in the | Devonian period 350 million years ago. |
ric lobe-finned fishes which lived during the | Devonian period (Famennian stage, about 374 to 359 mil |
t were formed by Hercynian folding during the | Devonian period of geological history. |
ough they do not become common until the Late | Devonian period in the latter half of the Paleozoic er |
of the Old Red Sandstone laid down during the | Devonian period but there is little rock exposed at th |
ated to be 395 ± 25 million years (during the | Devonian Period). |
Prior to the late | Devonian period, there was little plant life beyond li |
ily of placoderm fishes that lived during the | Devonian period, mainly in Norway and North America. |
It emerged very early during the Early | Devonian Period, around 400 million years ago, when ea |
med from Old Red Sandstone originating in the | Devonian period, specifically the sandstones of the Br |
are limited to the Eifelian age of the middle | Devonian Period, which occurred 398-391 million years |
first species of the genus lived in the later | Devonian period, and they survived until the end of th |
By the | Devonian Period, however, Ural Ocean begins to shrink |
tinct jawless fish that lived during the Late | Devonian period, similar to that of living lampreys fo |
to the Old Red Sandstone laid down during the | Devonian period. |
an to the Permian and were most common in the | Devonian period. |
us of lobe-finned fish which lived during the | Devonian period. |
inct genus of lungfish which lived during the | Devonian period. |
prehistoric lungfishes that lived during the | Devonian period. |
xtinct genus of prehistoric lungfish from the | Devonian period. |
coderm fish which existed in China during the | Devonian period. |
the Appalachian Basin area during the Middle | Devonian period. |
f prehistoric lungfish which lived during the | Devonian period. |
lobe-finned fish which lived during the Late | Devonian period. |
inct genus of lungfish which lived during the | Devonian period. |
us Limestone places it in the Early to Middle | Devonian period. |
Red Sandstone which was laid down during the | Devonian period. |
olepiform lobe-finned fish which lived during | Devonian period. |
enus of placoderm fish which lived during the | Devonian period. |
xtensive fossil record that starts during the | Devonian period. |
inct genus of lungfish which lived during the | Devonian period. |
storic lobe-finned fish that lived during the | Devonian period. |
ns which date from the Breconian stage of the | Devonian period. |
om the Old Red Sandstone laid down during the | Devonian period. |
ich lived between the Late Silurian and Early | Devonian period. |
s of primitive jawless fish that lived in the | Devonian period. |
Old Red Sandstone rocks laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
ite of sedimentary rocks laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
Red Sandstone which were laid down during the | Devonian period. |
s of primitive jawless fish that lived in the | Devonian period. |
ion of the Old Red Sandstone laid down in the | Devonian period. |
h hypocercal tails that lived during the Late | Devonian Period. |
of the Old Red Sandstone laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
of the Old Red Sandstone laid down during the | Devonian period. |
Tarsopterella dates from the Lower | Devonian period. |
It dates to the | Devonian period. |
tween the Carboniferous and the Silurian: the | Devonian Period. |
Red Sandstone which was laid down during the | Devonian period. |
lichopterids, which lived in the Silurian and | Devonian periods, were medium-sized, and had outer sur |
of bryozoan from the Ordovician, Silurian and | Devonian periods. |
ypterids are found from the Ordovician to the | Devonian periods. |
Ctenopterus date from the Silurian to the | Devonian periods. |
errestrial vascular plants of the Silurian to | Devonian periods. |
Sciadophyton is a lower | Devonian plant known from the Rhynie chert. |
Orestovia is a lower-middle | Devonian plant known from cuticle, which bears stomata |
Sudermann of Fortune Resorts; Stephen Ross of | Devonian Properties in Canmore; and Jeff Kohn of Calga |
ck types at the top of the river there is the | Devonian Quartzite(Metamorphic), in the middle of the |
iverged from sharks before the Chondrichthyan | Devonian radiation. |
arge but not particularly high and built in a | Devonian rather than a Cornish style. |
found in older Cretaceous, Mississippian, and | Devonian reservoirs. |
e) in London, assigning an age of 370 Ma to a | Devonian rock from Norway. |
iary volcano, whose cone is composed of Lower | Devonian rock and whose summit is made of basalt. |
of the Lynton Beds that are among the oldest | Devonian rocks in north Devon and are highly fossilife |
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