Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-25T10:18:14.689Z Has data issue: false hasContentIssue false
  • English
  • Français

The youngest cambroclaves: Cambroclavus absonus from the Middle Cambrian of the Cantabrian Zone (northwest Spain)

Published online by Cambridge University Press:  20 May 2016

Thomas Wotte
Thomas Wotte*
Affiliation:
Geologisch-Paläontologisches Institut, Westfalische-Wilhelms Universität Münster, Corrensstrasse 24, D-48149 Münster, Germany,
Get access Rights & Permissions [Opens in a new window]

Extract

Cambroclayes are Cambrian phosphatized problematica. The group is known from spine-like remains that are locally abundant on a number of Cambrian paleocontinents. Cambroclaves are known through a relatively short time interval (late Early Cambrian-early Middle Cambrian) mostly from tropical, carbonate platform successions on the Siberian Platform, East Gondwana (Australia, China, Kazakhstan), and West Gondwana. The West Gondwana occurrences include Cambroclavus ludwigsdorfensis Elicki, 1994 and Cambroclavus sp. from the late Early Cambrian of eastern Germany (Elicki, 1994, 2005; Elicki and Watte, 2003), and Cambroclavus sp. from the early Middle Cambrian of Sardinia (Elicki and Wotte, 2003;“ Elicki et al., 2003; Elicki, 2005, 2006). Recently, Clausen and Alvaro (2006) reported the zhijinitid form Parazhijinites cf. guizhouensis Qian and Yin, 1984 from the early Middle Cambrian of the Cantabrian zone of northwest Spain. Other than the mentioned tropical occurrences, Landing (1991) published the obviously cool to cold water form Samsanoffoclavus matthewi Landing, 1991 from the middle Early Cambrian of Cape Breton Island (Avalonia).

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 83 , Issue 1 , January 2009 , pp. 128 - 134
Copyright
Copyright © The Paleontological Society

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Álvaro, J. J. and Vizcaïno, D. 2003. The conocoryphid biofacies: A benthic assemblage of normal-eyed and blind trilobites. Special Papers in Palaeontology, 70:127–140.Google Scholar
Álvaro, J. J., Vizcaïno, D., and Vennin, E. 1999. Trilobite diversity patterns in the Middle Cambrian of southwestern Europe: A comparative study. Palaeogeography, Palaeoclimatology, Palaeoecology, 151:241–254.CrossRefGoogle Scholar
Álvaro, J. J., Vennin, E., Moreno-Eiris, E., Perejón, A., and Bechstädt, T. 2000. Sedimentary patterns across the Lower-Middle Cambrian transition in the Esla nappe (Cantabrian Mountains, northern Spain). Sedimentary Geology, 137:43–61.CrossRefGoogle Scholar
Babcock, L. E. and Peng, S. 2007. Cambrian chronostratigraphy: Current state and future plans. Palaeogeography, Palaeoclimatology, Palaeoecology, 254:62–66.CrossRefGoogle Scholar
Boogaard, M., Van Den, 1983. The occurrence of Hadimopanella oezgueli Gedik in the Láncara Formation in NW Spain. Palaeontology, 86:331–341.Google Scholar
Clausen, S. and Alvaro, J. J. 2006. Skeletonized microfossils from the Lower-Middle Cambrian transition of the Cantabrian Mountains, northern Spain. Acta Palaeontologica Polonica, 51:223–238.Google Scholar
Conway Morris, S. 1990. Cambroclaves, p. 103–119. In Bengtson, S., Conway Morris, S., Cooper, B. J., Jell, P. A., and Runnegar, B. N. (eds.), Early Cambrian fossils from South Australia. Memoir 9 of the Association of Australasian Palaeontologists, Brisbane.Google Scholar
Conway Morris, S. and Menge, C. 1991. Cambroclaves and paracarinachitids, early skeletal problematica from the Lower Cambrian of south China. Palaeontology, 34:357–397.Google Scholar
Conway-Morris, S., Crampton, J. S., Bing, Xiao, and Chapman, A. J. 1997. Lower Cambrian cambroclaves (incertae sedis) from Xinjiang, China, with comments on the morphological variability of sclerites. Palaeontology, 40:167–189.Google Scholar
Debrenne, F. and ZamarreñO., I. 1970. Sur le découverte d'Archéocyathes dans le Cambrien du NW de l'Espagne. Breviore Geologica Asturia, 14:1–11.Google Scholar
Duan, C. 1984. [date of imprint 1983]. Small shelly fossils from the Lower Cambrian Xihaoping Formation in the Shennongjia district, Hubei province—hyoliths and fossil skeletons of unknown affinities. Bulletin of the Tianjin Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 7:143–188. (In Chinese)Google Scholar
Elicki, O. 1994. Lower Cambrian carbonates from eastern Germany: Palaeontology, stratigraphy and palaeogeography. Neues Jahrbuch für Geologie und Paläontologie—Abhandlungen, 191:69–93.Google Scholar
Elicki, O. 2005. The utility of late Early to Middle Cambrian small shelly fossils from the western Mediterranean. Geosciences Journal, 9:161–171.CrossRefGoogle Scholar
Elicki, O. 2006. Microbiofacies analysis of Cambrian offshore carbonates from Sardinia (Italy): environment reconstruction and development of a drowning carbonate platform. Carnet de Géologie/Notebooks on Geology, 2006/01:1–22.Google Scholar
Elicki, O. and Wotte, T. 2003. Cambroclaves from the Cambrian of Sardinia (Italy) and Germany: Constraints for the architecture of western Gondwana and the palaeogeographical and palaeoecological potential of cambroclaves. Palaeogeography, Palaeoclimatology, Palaeoecology, 195: 55–71.CrossRefGoogle Scholar
Elicki, O., Hamann, Y., and Münzberger, P. 2003. Biofazies, Paläoökologie und Ablagerungsmodell des Finalstadiums einer kambrischen Karbonatplattform-Entwicklung: die Fauna der Campo Pisano Formation SW-Sardiniens. Freiberger Forschungshefte, C 499, Paläontologie, Stratigraphie, Fazies, 11:1–33.Google Scholar
Geyer, G. 1986. Mittelkambrische Mollusken aus Marokko und Spanien. Senckenbergiana lethaea, 67:55–118.Google Scholar
Geyer, G. and Landing, E. 2004. A unified Lower-Middle Cambrian chronostratigraphy for West Gondwana. Acta Geologica Polonica, 54:179–218.Google Scholar
Landing, E. 1991. Upper Precambrian through Lower Cambrian of Cape Breton Island: Faunas, paleoenvironments, and stratigraphic revision. Journal of Paleontology, 65:570–595.CrossRefGoogle Scholar
Liñán, E., Perejón, A., and Sdzuy, K. 1993. The Lower-Middle Cambrian tages and stratotypes from the Iberian Peninsula: A revision. Geological Magazine, 130:817–833.CrossRefGoogle Scholar
Mambetov, A. M. and Repina, L. N. 1979. The Lower Cambrian of Talasskiy Alatau and its correlation with the sections of Maly Karatau and the Siberian Platform. Trudy Instituta geologii i geofiziki. Sibirskoe Otdelenie. Akademija Nauk SSSR, 406:98–138. (In Russian)Google Scholar
Perejón, A. 1986. Bioestratigrafía de los arqueociatos en España. Cuadernos der Geología Ibérica, 9:213–265.Google Scholar
Perejón, A. 1994. Palaeogeographic and biostratigraphic distribution of Archaeocyatha in Spain. Courier Forschungsinstitut Senckenberg, 172:341–354.Google Scholar
Perejón, A. and Moreno-Eiris, E. 2003. Arqueociatos del Bilbiliense (Cámbrico Inferior) del manto del Esla, Cordillera Cantábrica, Norte de España. Boletin de la Real Sociedad Española de Historia Natural, Sección Geológica, 98:51–71.Google Scholar
Pérez-estaún, A., Bastida, F., Alonso, J. L., Marquínez, J., Aller, J., Alvarez-Marrón, J., Marcos, A., and Pulgar, J. A. 1988. A thin-skinned tectonics model for an arcuate fold and thrust belt: The Cantabrian Zone (Variscan Ibero-Armorican Arc). Tectonics, 7:517–537.CrossRefGoogle Scholar
Qian, Y. 1978. The early Cambrian hyolithids in central and southwestern China and their stratigraphical significance. Memoirs of the Nanjing Institute of Geology and Palaeontology, 11:1–38. (In Chinese)Google Scholar
Qian, Y. and Yin, G.-Z. 1984. Zhijinitidae and its stratigraphical significance. Acta Paleontologica Sinica, 23:215–223. (In Chinese)Google Scholar
Quian, Y. and Zhang, S. 1983. Small shelly fossils from the Xihanoping Member of the Tongying Formation in Fangxian County of Hubei Province and their stratigraphical significance. Acta Palaeontologica Sinica, 22:82–94. (In Chinese)Google Scholar
Sdzuy, K. 1958. Neue Trilobiten aus dem Mittelkambrium von Spanien. Senckenbergiana lethaea, 39:235–253.Google Scholar
Sdzuy, K. 1968. Biostratigrafia de la griotte Cambrica de Los Barrios de Luna (Leon) y de otras sucesiones comparables. Trabajos de Geología, 2: 45–58.Google Scholar
Sdzuy, K. 1974. Mittelkambrische Graptolithen aus NW-Spanien. Paläontologische Zeitschrift, 48:110–139.CrossRefGoogle Scholar
Sdzuy, K. 1995. Acerca del conocimiento actual del Sistema Cámbrico y del Límite Cámbrico Inferior–Medio en España, p. 253–264. In Liñán, E. and Gámez-Vintaned, J. A. (eds.), Memorias de las IV Jornados Aragonesas de Paleontología: “La expansion de la vida en el Cámbrico.” Libro homenaje al Prof. Klaus Sdzuy. Institucíon “Fernando el Católico” Press, Zaragoza.Google Scholar
Thoral, M. 1946. Conocoryphidae languedociens. Annales de l'Université de Lyon, Sciences Naturelles, 4:5–92.Google Scholar
Wotte, T. 2005. Facies distribution patterns of the upper member of the Láncara Formation in the Somiedo-Correcilla unit (Lower-Middle Cambrian, Cantabrian zone, NW Spain) with special respect to biofacial investigations. Geosciences Journal, 9:389–402.CrossRefGoogle Scholar
Wotte, T. 2006. New Middle Cambrian molluscs from the Láncara Formation of the Cantabrian Mountains (north-western Spain). Revista Española de Paleontología, 21:145–158.Google Scholar
Wotte, T. and Mergl, M. 2007. Brachiopods from the Lower-Middle Cambrian Láncara Formation of the Cantabrian Mountains (NW Spain). Memoirs of the Association of Australasian Palaeontologists, 33:101–122.Google Scholar
Wotte, T., Elicki, O., Perejón, A., and Moreno-Eiris, E. 2004. Facies distribution patterns and environment interpretation of the Upper Láncara Formation in the Esla Nappe (Cantabrian zone, NW Spain) by quantitative microfacies analysis. Freiberger Forschungshefte, C 502, Paläontologie, Stratigraphie, Fazies, 12:101–118.Google Scholar
Wotte, T., ÁLvaro, J. J., Shields, G. A., Brown, B., Brasier, M., and Veizer, J. 2007. C-, O- and Sr-isotope stratigraphy across the Lower-Middle Cambrian transition of the Cantabrian zone (Spain) and the Montagne Noire (France), West Gondwana. Palaeogeography, Palaeoclimatology, Palaeoecology, 256:47–70.CrossRefGoogle Scholar
ZamarreñO, I. 1972. Las litofacies carbonatadas del Cámbrico de la Zona Cantábrica (NW de España) y su distribución paleogeográfica. Trabajos de Geología, 5:1–118.Google Scholar
ZamarreñO, I. and Julivert, M. 1968. Estratigrafía del Cámbrico del Oriente de Asturias y studio petrográfico de las facies carbonatadas. Trabajos de Geología, 1:135–163.Google Scholar