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Ladinian

The Ladinian is a stage and age in the Middle Triassic series or epoch. It spans the time between 242 Ma and ~237 Ma (million years ago).[8] The Ladinian was preceded by the Anisian and succeeded by the Carnian (part of the Upper or Late Triassic).[9]

Ladinian
~242 – ~237 Ma
Monte San Giorgio exhibits exceptionally preserved Ladinian vertebrate fossils
Chronology
Etymology
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionFAD of the Ammonite Eoprotrachyceras curionii
Lower boundary GSSPBagolino, Lombardian pre-Alps, Italy
45°49′09″N 10°28′16″E / 45.8193°N 10.4710°E / 45.8193; 10.4710
Lower GSSP ratified2005[6]
Upper boundary definitionFAD of the Ammonite Daxatina canadensis
Upper boundary GSSPPrati di Stuores, Dolomites, Italy
46°31′37″N 11°55′49″E / 46.5269°N 11.9303°E / 46.5269; 11.9303
Upper GSSP ratified2008[7]

The Ladinian is coeval with the Falangian regional stage used in China.

Stratigraphic definitions

 
The GSSP of the Ladinian at Bagolino in Italy

The Ladinian was established by Austrian geologist Alexander Bittner in 1892. Its name comes from the Ladin people that live in the Italian Alps (in the Dolomites, then part of Austria-Hungary).

The base of the Ladinian Stage is defined as the place in the stratigraphic record where the ammonite species Eoprotrachyceras curionii first appears or the first appearance of the conodont Budurovignathus praehungaricus. The global reference profile for the base (the GSSP) is at an outcrop in the river bed of the Caffaro river at Bagolino, in the province of Brescia, northern Italy.[10] The top of the Ladinian (the base of the Carnian) is at the first appearance of ammonite species Daxatina canadensis.

The Ladinian is sometimes subdivided into two subages or substages, the Fassanian (early or lower) and the Longobardian (late or upper). The Ladinian contains four ammonite biozones, which are evenly distributed among the two substages:

Ladinian life

Notable formations

* Tentatively assigned to the Ladinian; age estimated primarily via terrestrial tetrapod biostratigraphy (see Triassic land vertebrate faunachrons)

References

Notes

  1. ^ Widmann, Philipp; Bucher, Hugo; Leu, Marc; et al. (2020). "Dynamics of the Largest Carbon Isotope Excursion During the Early Triassic Biotic Recovery". Frontiers in Earth Science. 8 (196): 196. Bibcode:2020FrEaS...8..196W. doi:10.3389/feart.2020.00196.
  2. ^ McElwain, J. C.; Punyasena, S. W. (2007). "Mass extinction events and the plant fossil record". Trends in Ecology & Evolution. 22 (10): 548–557. doi:10.1016/j.tree.2007.09.003. PMID 17919771.
  3. ^ Retallack, G. J.; Veevers, J.; Morante, R. (1996). "Global coal gap between Permian–Triassic extinctions and middle Triassic recovery of peat forming plants". GSA Bulletin. 108 (2): 195–207. Bibcode:1996GSAB..108..195R. doi:10.1130/0016-7606(1996)108<0195:GCGBPT>2.3.CO;2. Retrieved 2007-09-29.
  4. ^ Payne, J. L.; Lehrmann, D. J.; Wei, J.; Orchard, M. J.; Schrag, D. P.; Knoll, A. H. (2004). "Large Perturbations of the Carbon Cycle During Recovery from the End-Permian Extinction". Science. 305 (5683): 506–9. Bibcode:2004Sci...305..506P. doi:10.1126/science.1097023. PMID 15273391. S2CID 35498132.
  5. ^ Ogg, James G.; Ogg, Gabi M.; Gradstein, Felix M. (2016). "Triassic". A Concise Geologic Time Scale: 2016. Elsevier. pp. 133–149. ISBN 978-0-444-63771-0.
  6. ^ Brack, Peter; Rieber, Hans; Nicora, Alda; Mundil, Roland (December 2005). "The Global boundary Stratotype Section and Point (GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and its implications for the Triassic time scale". Episodes. 28 (4): 233–244. doi:10.18814/epiiugs/2005/v28i4/001. Retrieved 23 December 2020.
  7. ^ Mietto, Paolo; Manfrin, Stefano; Preto, Nereo; Rigo, Manuel; Roghi, Guido; Furin, Stefano; Gianolla, Piero; Posenato, Renato; Muttoni, Giovanni; Nicora, Alda; Buratti, Nicoletta; Cirilli, Simonetta; Spötl, Christoph; Ramezani, Jahandar; Bowring, Samuel (September 2012). "The Global Boundary Stratotype Section and Point (GSSP) of the Carnian Stage (Late Triassic) at Prati Di Stuores/Stuores Wiesen Section (Southern Alps, NE Italy)" (PDF). Episodes. 35 (3): 414–430. doi:10.18814/epiiugs/2012/v35i3/003. Retrieved 13 December 2020.
  8. ^ "Chart". International Commission on Stratigraphy. Retrieved 20 February 2022.
  9. ^ For a detailed geologic timescale see Gradstein et al. (2004)
  10. ^ The GSSP was established by Brack et al. (2005)

Literature

  • Brack, P.; Rieber, H.; Nicora, A. & Mundil, R.; 2005: The Global boundary Stratotype Section and Point (GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and its implications for the Triassic time scale, Episodes 28(4), pp. 233–244.
  • Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.

External links

  • GeoWhen Database - Ladinian 2010-08-22 at the Wayback Machine
  • Upper Triassic and Lower Triassic timescales, at the website of the subcommission for stratigraphic information of the ICS
  • Norges Network of offshore records of geology and stratigraphy: Stratigraphic charts for the Triassic, and

Coordinates: 45°49′09″N 10°28′16″E / 45.8193°N 10.4710°E / 45.8193; 10.4710

ladinian, stage, middle, triassic, series, epoch, spans, time, between, million, years, preceded, anisian, succeeded, carnian, part, upper, late, triassic, preꞒ, monte, giorgio, exhibits, exceptionally, preserved, vertebrate, fossilschronology, pzmesozoicptria. The Ladinian is a stage and age in the Middle Triassic series or epoch It spans the time between 242 Ma and 237 Ma million years ago 8 The Ladinian was preceded by the Anisian and succeeded by the Carnian part of the Upper or Late Triassic 9 Ladinian 242 237 Ma PreꞒ Ꞓ O S D C P T J K Pg N Monte San Giorgio exhibits exceptionally preserved Ladinian vertebrate fossilsChronology 255 250 245 240 235 230 225 220 215 210 205 200 PzMesozoicPTriassicJEarMiddleLateEJChanghsing OlenekianInduanAnisianLadinianCarnianNorianRhaetianHettangian Permian Triassic extinction event Smithian Spathian boundary event 1 Carnian pluvial episode Full recovery of woody trees 2 Coals return 3 Scleractiniancorals amp calcified sponges 4 Triassic Jurassic extinction event Manicouagan impactSubdivision of the Triassic according to the ICS as of 2021 5 Vertical axis scale millions of years ago EtymologyName formalityFormalUsage informationCelestial bodyEarthRegional usageGlobal ICS Time scale s usedICS Time ScaleDefinitionChronological unitAgeStratigraphic unitStageTime span formalityFormalLower boundary definitionFAD of the Ammonite Eoprotrachyceras curioniiLower boundary GSSPBagolino Lombardian pre Alps Italy45 49 09 N 10 28 16 E 45 8193 N 10 4710 E 45 8193 10 4710Lower GSSP ratified2005 6 Upper boundary definitionFAD of the Ammonite Daxatina canadensisUpper boundary GSSPPrati di Stuores Dolomites Italy46 31 37 N 11 55 49 E 46 5269 N 11 9303 E 46 5269 11 9303Upper GSSP ratified2008 7 The Ladinian is coeval with the Falangian regional stage used in China Contents 1 Stratigraphic definitions 2 Ladinian life 3 Notable formations 4 References 4 1 Notes 4 2 Literature 5 External linksStratigraphic definitions Edit The GSSP of the Ladinian at Bagolino in Italy The Ladinian was established by Austrian geologist Alexander Bittner in 1892 Its name comes from the Ladin people that live in the Italian Alps in the Dolomites then part of Austria Hungary The base of the Ladinian Stage is defined as the place in the stratigraphic record where the ammonite species Eoprotrachyceras curionii first appears or the first appearance of the conodont Budurovignathus praehungaricus The global reference profile for the base the GSSP is at an outcrop in the river bed of the Caffaro river at Bagolino in the province of Brescia northern Italy 10 The top of the Ladinian the base of the Carnian is at the first appearance of ammonite species Daxatina canadensis The Ladinian is sometimes subdivided into two subages or substages the Fassanian early or lower and the Longobardian late or upper The Ladinian contains four ammonite biozones which are evenly distributed among the two substages zone of Frechites regoledanus zone of Protrachyceras archelaus zone of Protrachyceras gredleri zone of Eoprotrachyceras curioniiLadinian life EditMain page Category Ladinian lifeNotable formations EditBukobay Svita Russia Erfurt Formation Lower Keuper Germany Jilh Formation Saudi Arabia Meride Limestone Switzerland and Italy Upper Muschelkalk central Europe Perledo Varenna Formation Italy Prosanto Formation Switzerland Lower Santa Maria Formation late Ladinian early Carnian Rio Grande do Sul Brazil Zhuganpo Formation Zhuganpo Member of the Falang Formation late Ladinian early Carnian Guizhou and Yunnan China Tentatively assigned to the Ladinian age estimated primarily via terrestrial tetrapod biostratigraphy see Triassic land vertebrate faunachrons References EditNotes Edit Widmann Philipp Bucher Hugo Leu Marc et al 2020 Dynamics of the Largest Carbon Isotope Excursion During the Early Triassic Biotic Recovery Frontiers in Earth Science 8 196 196 Bibcode 2020FrEaS 8 196W doi 10 3389 feart 2020 00196 McElwain J C Punyasena S W 2007 Mass extinction events and the plant fossil record Trends in Ecology amp Evolution 22 10 548 557 doi 10 1016 j tree 2007 09 003 PMID 17919771 Retallack G J Veevers J Morante R 1996 Global coal gap between Permian Triassic extinctions and middle Triassic recovery of peat forming plants GSA Bulletin 108 2 195 207 Bibcode 1996GSAB 108 195R doi 10 1130 0016 7606 1996 108 lt 0195 GCGBPT gt 2 3 CO 2 Retrieved 2007 09 29 Payne J L Lehrmann D J Wei J Orchard M J Schrag D P Knoll A H 2004 Large Perturbations of the Carbon Cycle During Recovery from the End Permian Extinction Science 305 5683 506 9 Bibcode 2004Sci 305 506P doi 10 1126 science 1097023 PMID 15273391 S2CID 35498132 Ogg James G Ogg Gabi M Gradstein Felix M 2016 Triassic A Concise Geologic Time Scale 2016 Elsevier pp 133 149 ISBN 978 0 444 63771 0 Brack Peter Rieber Hans Nicora Alda Mundil Roland December 2005 The Global boundary Stratotype Section and Point GSSP of the Ladinian Stage Middle Triassic at Bagolino Southern Alps Northern Italy and its implications for the Triassic time scale Episodes 28 4 233 244 doi 10 18814 epiiugs 2005 v28i4 001 Retrieved 23 December 2020 Mietto Paolo Manfrin Stefano Preto Nereo Rigo Manuel Roghi Guido Furin Stefano Gianolla Piero Posenato Renato Muttoni Giovanni Nicora Alda Buratti Nicoletta Cirilli Simonetta Spotl Christoph Ramezani Jahandar Bowring Samuel September 2012 The Global Boundary Stratotype Section and Point GSSP of the Carnian Stage Late Triassic at Prati Di Stuores Stuores Wiesen Section Southern Alps NE Italy PDF Episodes 35 3 414 430 doi 10 18814 epiiugs 2012 v35i3 003 Retrieved 13 December 2020 Chart International Commission on Stratigraphy Retrieved 20 February 2022 For a detailed geologic timescale see Gradstein et al 2004 The GSSP was established by Brack et al 2005 Literature Edit Brack P Rieber H Nicora A amp Mundil R 2005 The Global boundary Stratotype Section and Point GSSP of the Ladinian Stage Middle Triassic at Bagolino Southern Alps Northern Italy and its implications for the Triassic time scale Episodes 28 4 pp 233 244 Gradstein F M Ogg J G amp Smith A G 2004 A Geologic Time Scale 2004 Cambridge University Press External links EditGeoWhen Database Ladinian Archived 2010 08 22 at the Wayback Machine Upper Triassic and Lower Triassic timescales at the website of the subcommission for stratigraphic information of the ICS Norges Network of offshore records of geology and stratigraphy Stratigraphic charts for the Triassic 1 and 2 Coordinates 45 49 09 N 10 28 16 E 45 8193 N 10 4710 E 45 8193 10 4710 Retrieved from https en wikipedia org w index php title Ladinian amp oldid 1137843470, wikipedia, wiki, book, books, library,

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