Cambrian Evolutionary Radiation: Context, correlation, and chronostratigraphy—Overcoming deficiencies of the first appearance datum (FAD) concept

作者: Ed Landing , Gerd Geyer , Martin D. Brasier , Samuel A. Bowring

DOI: 10.1016/J.EARSCIREV.2013.03.008

关键词: ChronostratigraphyFirst appearance datumDiachronousTrace fossilGlobal Boundary Stratotype Section and PointAcritarchHeterochronyPaleontologyGeologyEvolutionary radiation

摘要: Abstract Use of the first appearance datum (FAD) a fossil to define global chronostratigraphic unit's base can lead intractable correlation and stability problems. FADs are diachronous—they reflect species' evolutionary history, dispersal, biofacies, preservation, collection, taxonomy. The Cambrian Evolutionary Radiation is characterised by diachronous FADs, biofacies controls, provincialism taxa ecological communities that confound stable Lower chronostratigraphy. series stage definitions require greater attention assemblage zone successions non-biostratigraphic, particularly carbon isotope, techniques such as those Ediacaran System base. A redefined, basal Trichophycus pedum Assemblage Zone lies above highest Ediacaran-type biotas (vendobionts, putative metazoans, calcareous problematica Cloudina ) Asteridium tornatum–Comasphaeridium velvetum (acritarchs). This definition likely close correspondence origin local FAD T. preserves Fortune Head, Newfoundland, GSSP allows presence sub-Cambrian, branched ichnofossils. sub-Tommotian-equivalent Stage 2 (a suggested “Laolinian Stage”) should be defined I′/L4/ZHUCE δ 13 C positive peak, bracketed lower ranges Watsonella crosbyi Aldanella attleborensis (molluscs) Skiagia ornata–Fimbrioglomerella membranacea W. A. cannot they even in Newfoundland “type” Zone. Series based on owing skeletalised metazoans Terreneuvian–Series boundary interval heterochrony oldest trilobites. 3 “Lenaldanian Series” “Zhurinskyan Stage,” new) proposed at Siberian Atdabanian IV peak—which correlates into South China, Avalonia, Morocco assigns trilobites terminal Terreneuvian Series.

参考文章(251)
E. S. Cobbold, Additional Fossils from the Cambrian Rocks of Comley, Shropshire Quarterly Journal of The Geological Society. ,vol. 87, pp. 459- 512 ,(1931) , 10.1144/GSL.JGS.1931.087.01-04.17
Ed Landing, Samuel A Bowring, Kathleen L Davidek, Stephen R Westrop, Gerd Geyer, Wolfram Heldmaier, Duration of the Early Cambrian: U-Pb ages of volcanic ashes from Avalon and Gondwana Canadian Journal of Earth Sciences. ,vol. 35, pp. 329- 338 ,(1998) , 10.1139/E97-107
FREDRIK TERFELT, GABRIELLA BAGNOLI, SVEND STOUGE, Re‐evaluation of the conodont Iapetognathus and implications for the base of the Ordovician System GSSP Lethaia. ,vol. 45, pp. 227- 237 ,(2012) , 10.1111/J.1502-3931.2011.00275.X
Ed Landing, Stephen R. Westrop, Upper Lower Cambrian depositional sequence in Avalonian New Brunswick Canadian Journal of Earth Sciences. ,vol. 33, pp. 404- 417 ,(1996) , 10.1139/E96-030
ARTEM KOUCHINSKY, STEFAN BENGTSON, BRUCE RUNNEGAR, CHRISTIAN SKOVSTED, MICHAEL STEINER, MICHAEL VENDRASCO, Chronology of early Cambrian biomineralization Geological Magazine. ,vol. 149, pp. 221- 251 ,(2012) , 10.1017/S0016756811000720
JONATHAN B. ANTCLIFFE, ANDREW J. GOODAY, MARTIN D. BRASIER, Testing the protozoan hypothesis for Ediacaran fossils: a developmental analysis of Palaeopascichnus Palaeontology. ,vol. 54, pp. 1157- 1175 ,(2011) , 10.1111/J.1475-4983.2011.01058.X
E. Mayoral, R. Gozalo, T. Palacios, J. A. Gámez Vintaned, E. Liñán, The Cambrian of the Iberian Peninsula: An overview Geologica Acta. ,vol. 1, pp. 103- 112 ,(2003) , 10.1344/105.000001596