Geragnostus

Geragnostus ; Временный диапазон: Ордовик ( Tremadocian to Ashgill ) Предварительный Ꞓ А С Дюймовый В П Т Дж K Пг Не
	Geragnostus mediterraneus, 6mm, St.Chinian Formation, France, Middle Ordovician
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Arthropoda
Class:	†Trilobita (?)
Order:	†Agnostida
Family:	†Metagnostidae
Genus:	†Geragnostus; Howell, 1935
Species
	G. sidenbladhi (Linnarsson, 1869) (type) synonym Agnostus sidenbladhi; G. balanolobus Turvey, 2005; G. clusus Whittington, 1963; G. consors (Holub, 1912) synonyms Agnostus consors, Neptunagnostella consors; G. crassus Tjernvik, 1956; G. fabius Billings, 1865; G. fenhsiangensis Lu, 1975; G. gilcidae Rábano, Pek & Vaněk, 1985; G. hispanicus Rábano, Pek & Vaněk, 1985; G. kirgizica (Weber, 1948) synonyms Trinodus glabratus var. kirgizica, T. kirgizica; G. longicollis Raymond, 1925; G. occitanus Howell, 1935; G. perconvexus (Kobayashi & Hamada, 1978) synonym Geratrinodus perconvexus; G. splendens (Holub, 1912); G. tullbergi (Novák, 1883) synonyms Agnostus tullbergi, Geragnostella tullbergi; G. waldorfstatleri Turvey, 2005;
Synonyms
	Geragnostella, Geratrinodus, Neptunagnostella

Geragnostus -это род очень маленьких агностидных трилобитов , окаменелости которых найдены с ордовиком морские слои из Евразии , Северной Америки и Аргентины .

Этимология

Balanolobus получен из греческого «Баланоса», Acorn и «Lobos», доли, в отношении контура задней доли Rhachis.
Я пиладиш
Waldorfstatleri назван в честь Muppets Statler и Waldorf за подобие Rhachis с головами. ^{[ 3 ]}

Таксономия

Geragnostus очень похож на Trinodus и может быть включен в этот род. В Тринодусе задняя доля (M3) пигидиальной оси (или Rhachis) явно короче, чем передние и средние доли (M1+M2), в то время как в Geragnostus она равна или больше по длине. Geragnostus не тесно связан с Micragnostus , потому что его глабелла структурно отличается. ^[4]

Species previously assigned to Geragnostus

G. chronius = Oncagnostus (Strictagnostus) chronius
G. hirundo = Segmentagnostus hirundo
G. scoltonensis = Segmentagnostus scoltonensis

Distribution

G. clusus, was found in the Middle Ordovician of Canada (Llanvirn, Lower Head, Newfoundland)^[3]
G. crassus, has been identified from the Lower Ordovician of Baltica (Tremadoc), and the Lower (Tremadoc of Yingou, Yumen County, Gansu) and Middle Ordovician of China (lower Llanvirn, Angzhanggou, Yumen County, Gansu)^[3]
G. fabius, Canada (Newfoundland and Labrador)^[5]
G. fenhsiangensis, is known from the Middle Ordovician of China (Dawan Formation, upper Arenig, Fenxiang, Yichang County, West Hubei)^[3]
G. gilcidae and G. hispanicus, were found in the Middle Ordovician of Spain (lower Llanvirn, Southern Central-Iberian Zone, Mounts of Toledo, Villuercas and Almadén district)
G. kirgizica, is present in the Middle Ordovician of Kazakhstan (Karakansky horizon), and the Upper Ordovician of Iran (late Caradoc, early Asgill, Tatavrud, 35 km southwest of Bandar-e-Anzali)^[1]
G. longicollis, in Canada and China^[6]
G. occitanus, is present in the Lower and Middle Ordovician of France (Arenig, Montagne Noire)^[3]
G. sidenbladhi, occurs in the Lower Ordovician (upper Tremadoc, Ceratopyge-limestone, Apatokephalus serratus-biozone) of Sweden (Mossebo, Hunneberg, Västergötland; Fågelsång, Scania) and Norway (Trefoldighetskirken, central Oslo; Bjerkåsholmen, Slemmestad in the Oslo-Asker district; Fure at Tyrifjorden in the Modum district; and Samsal in the Ringsaker district)^[4]
G. splendens, was excavated from the Lower and Middle Ordovician of Baltica and the Czech Republic (Arenig)^[3]
G. waldorfstatleri, has been found in the Lower and Middle Ordovician of South China (Arenig-Llanvirn)^[3]

Unidentified species in the genus Geragnostus have among others been found in Colombia (Guaviare River, Meta).^[7]

Description

Like all Agnostida, Geragnostus is diminutive, with the headshield (or cephalon) and tailshield (or pygidium) of approximately the same size (or isopygous) and outline. Like all Agnostina, Geragnostus has only two thorax segments, where known. The cephalon is subquadrate in outline, and almost as long as wide. The highest point is the node in the centre of the centrally raised section of the cephalon (or glabella). The glabella is about 2⁄3 times the length of the cephalon, and its sides are very gently tapered forward, with a broadly rounded front, and is well defined by shallow furrows and an abrupt change in exoskeletal slope. It is 2 times as long as wide. The elongated glabellar node is prominent. The rear of the glabella is straight. Just in front of the node, a depression curves forward- and outward. The basal lobes are wider than they are long and almost touch. The border is relatively narrow, gently convex, and defined by a wide, shallow border furrow, widest at the front. The genal angles are pointed without spines.

The pygidial axis (or rhachis) is 1⁄2–2⁄3 times as long as the pygidium, almost parallel-sided, very slightly constricted at the middle lobe (M2), broadly rounded, and 1+1⁄3–1+2⁄3 times as long as wide. It has three distinct pairs of lobes, and is defined by shallow furrows. The forward lobe of the rhachis (M1) is a bit shorter and wider than the middle lobe (M2) and separated from it by a furrow (F1) which is directed outward and slightly backward from the dorsal furrow, and then curved strongly forward adaxially. The rear lobe (M3) is 1+1⁄3–1+2⁄3 longer than both others together, and the furrow is directed outward and slightly forward from the dorsal furrow. The middle lobe has a prominent tubercle, which extends backwards above the anterior portion of rear lobe. It is the highest point of the pygidium. The border is moderately wide, gently convex, defined by a shallow furrow, and widest at the rear corners which carry a pair of strong, backwardly directed spines.^[4]

References

^ Jump up to: ^a ^b Karim, T.S. (2009). "Ordovician trilobites from Iran". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 02 (99): 101–124. doi:10.1017/s1755691009007063. S2CID 129780250.
^ Whittington, H. B. et al. Part O, Treatise on Invertebrate Paleontology. Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida. 1997
^ Jump up to: ^a ^b ^c ^d ^e ^f ^g ^h Turvey, S.T. (2005). "Agnostid trilobites from the Arenig-Llanvirn of South China". Transactions of the Royal Society of Edinburgh: Earth Sciences. 95 (3–4): 527–542. doi:10.1017/s026359330000119x. S2CID 130775617.
^ Jump up to: ^a ^b ^c Альберг П. (1989). «Типовые виды ордовикского агностидного трилобита geragnostus , Howell, 1935». Палеонтологический журнал . 63 (3–4): 309–317. Bibcode : Palatinate 1989 ... 63..309a . Doi : 10.1007/bf02989517 . S2CID 85408131 .
^ Geragnostus fabius at fossilworks .org
^ Geragnostus longicollis at fossilworks .org
^ Ордовик реки Гуавиара на исчезающих заводах .

[Karim-1] Jump up to: ^a ^b Karim, T.S. (2009). "Ordovician trilobites from Iran". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 02 (99): 101–124. doi:10.1017/s1755691009007063. S2CID 129780250.

[Treatise-2] Whittington, H. B. et al. Part O, Treatise on Invertebrate Paleontology. Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida. 1997

[Turvey-3] Jump up to: ^a ^b ^c ^d ^e ^f ^g ^h Turvey, S.T. (2005). "Agnostid trilobites from the Arenig-Llanvirn of South China". Transactions of the Royal Society of Edinburgh: Earth Sciences. 95 (3–4): 527–542. doi:10.1017/s026359330000119x. S2CID 130775617.

[Ahlberg-4] Jump up to: ^a ^b ^c Альберг П. (1989). «Типовые виды ордовикского агностидного трилобита geragnostus , Howell, 1935». Палеонтологический журнал . 63 (3–4): 309–317. Bibcode : Palatinate 1989 ... 63..309a . Doi : 10.1007/bf02989517 . S2CID 85408131 .

[FWGeragnostusFabius-5] Geragnostus fabius at fossilworks .org

[FWGeragnostusLongicollis-6] Geragnostus longicollis at fossilworks .org

[FWGuaviare-7] Ордовик реки Гуавиара на исчезающих заводах .

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