New biostratigraphic framework for the Triassic–Paleogene in the Neo-Tethys realm of southern Xizang (Tibet), China

2020 ◽  
Vol 202 ◽  
pp. 104369 ◽  
Author(s):  
Jianguo Li ◽  
Miaoqin Lin ◽  
Yixiao Wu ◽  
Hui Luo ◽  
Jungang Peng ◽  
...  
Keyword(s):  
2015 ◽  
Vol 104 (6) ◽  
pp. 1679-1684 ◽  
Author(s):  
Luigi Beccaluva ◽  
Gianluca Bianchini ◽  
Massimo Coltorti ◽  
Claudio Natali
Keyword(s):  

2015 ◽  
Vol 104 (5) ◽  
pp. 1317-1336 ◽  
Author(s):  
Fabio Carmelo Manuella ◽  
Vittorio Scribano ◽  
Serafina Carbone ◽  
Alfonso Brancato
Keyword(s):  

2015 ◽  
Vol 104 (6) ◽  
pp. 1685-1691 ◽  
Author(s):  
Fabio Carmelo Manuella ◽  
Vittorio Scribano ◽  
Serafina Carbone ◽  
Alfonso Brancato
Keyword(s):  

Lethaia ◽  
1980 ◽  
Vol 13 (1) ◽  
pp. 92-92
Author(s):  
HELMUTH ZAPFE
Keyword(s):  

1994 ◽  
Vol 68 (S36) ◽  
pp. 1-33 ◽  
Author(s):  
George D. Stanley ◽  
Carlos González-León ◽  
Michael R. Sandy ◽  
Baba Senowbari-Daryan ◽  
Peter Doyle ◽  
...  

A diverse Upper Triassic tropical marine fauna from northwestern Sonora, Mexico, includes 31 taxa of tropical invertebrates including scleractinian corals, spongiomorphs, disjectoporoids, “hydrozoans,” thalamid and nonthalamid sponges, spiriferid and terebratulid brachiopods, gastropods, bivalves, coleoids, and anomuran microcoprolites. They occur within the late Karnian to Norian part of the Antimonio Formation (Antimonio terrane), which is juxtaposed against a fragmented portion of the North American craton. Most of the fauna is also known from the Tethys region. Sixteen Sonoran taxa co-occur in the western Tethys and five have never been known outside this region. Four additional taxa (one identified only at genus level) are geographically widespread. Some taxa occur in displaced terranes of North America, especially in west-central Nevada (Luning Formation). A weak link exists with the California Eastern Klamath terrane but stronger ties exist with Peru. Among Sonoran sponges,Nevadathalamia polystomawas previously recognized only from the Luning Formation, western Nevada. SpongesCinnabaria expansa, Nevadathalamia cylindrica, and a coral,Astraeomorpha sonorensisn. sp., are also known from Nevada. The coralsDistichomeandra austriaca, Chondrocoenia waltheri, Pamiroseris rectilamellosa, andAlpinophyllia flexuosaco-occur in central Europe. Two new taxa, a spongiomorph hydrozoan,Stromatoporidium lamellatumn. sp., and a disjectoporoid,Pamiropora sonorensisn. sp., have distinct affinities with the Tethys. The geographically widespread North American brachiopod,Spondylospira lewesensis, andPseudorhaetina antimoniensisn. gen. and sp. are among the Sonoran fauna. The Sonoran coleoid (aulacocerid)Dictyoconites(Dictyoconites) cf.D. reticulatumoccurs in the Tethys realm andCalliconitescf.C. drakeiis comparable with a species from the Eastern Klamath terrane.Calliconites millerin. sp. is the first occurrence of the genus outside Sicily. The bivalvesMyophorigonia jaworskii, M. salasi, andPalaeocardita peruvianaare known from Sonora and Peru. Eight gastropod taxa includeGuidoniacf.G. intermediaandG.cf.G. parvula, both previously known from Peru, andEucycloscala subbisertusfrom the western Tethys. The gastropods are unlike those already known from other North American terranes.


Tectonics ◽  
2011 ◽  
Vol 30 (3) ◽  
pp. n/a-n/a ◽  
Author(s):  
Dominique Frizon de Lamotte ◽  
Camille Raulin ◽  
Nicolas Mouchot ◽  
Jean-Christophe Wrobel-Daveau ◽  
Christian Blanpied ◽  
...  

2016 ◽  
Vol 67 (5) ◽  
pp. 451-462 ◽  
Author(s):  
Behnaz Kalanat ◽  
Mohammad Vahidinia ◽  
Hossein Vaziri-Moghaddam ◽  
Mohamad Hossein Mahmudy-Gharaie

Abstract Two Late Cenomanian – Early Turonian (C–T) intervals of the eastern part of the Kopet-Dagh basin, NE Iran have been investigated to evaluate the response of planktonic foraminifera to the geological event OAE2. The Gharesu and Taherabad sections with the thicknesses of 30 m and 22.5 m are composed of shale and marl interbedded with glauconitic sandstone. Three biozones Rotalipora cushmani, Whiteinella archaeocretacea and Helvetoglobotruncana helvetica were recognized based on study of planktonic foraminifera, in these sections. We observed the patterns of planktonic foraminiferal assemblage changes around the C–T boundary and divided this succession into several successive intervals. This study confirms that OAE2 was a long term event. A gradual perturbation in the study successions starts in the interval 1 with low abundance and diversity of planktonic foraminifera. An enhanced oxygen minimum zone (OMZ) occurs in the interval 3 which coincides with a temporary absence of planktonic foraminifera and sedimentation of framboidal pyrite. High diversity of planktonic foraminifera and appearance of new genera in the interval 5 indicate return of normal conditions to the basin. A significant short-term sea surface temperature cooling is also indicated by planktonic foraminiferal turnover and carbonate contents in the interval 2 which is comparable with other parts of the Tethys Ocean, Boreal sea and Atlantic region.


Sign in / Sign up

Export Citation Format

Share Document