The Icla Formation is an early Devonian formation from Bolivia. It preserves a moderately diverse fauna of trilobites, brachiopods, crinoids and a few species of jawed fish.
Also known from the Belèn Formation, one of the most basal known cartilaginous fish
Fossilized jaws and teeth of P. rodrigae (A-C, G-H) and cartilage elements of Zamponiopteron (D-F), which may belong to the same animal, from the Department of Puno, Peru. Scale bar = 0.5 cm
↑Pradel, Alan; Maisey, John G.; Tafforeau, P.; Janvier, Philippe (May 2009). "An enigmatic gnathostome vertebrate skull from the Middle Devonian of Bolivia". Acta Zoologica. 90 (s1): 123–133. doi:10.1111/j.1463-6395.2008.00350.x.
↑Maisey, John G.; Janvier, Philippe; Pradel, Alan; Denton, John S. S.; Bronson, Allison; Miller, Randall; Burrow, Carole J. (31 December 2018). "Doliodus and Pucapampellids: Contrasting Perspectives on Stem Chondrichthyan Morphology". Evolution and Development of Fishes: 87–109. doi:10.1017/9781316832172.006.
↑Scheffler, Sandro M. (January 2021). "Crinoids from the Lower (Pragian–Emsian) and Middle (early Eifelian) Devonian of Bolivia (Icla and Belén formations, Malvinokaffric Realm)". Journal of Paleontology. 95 (1): 141–153. doi:10.1017/jpa.2020.70.
12Thompson, Jeffrey R.; Ausich, William I.; Smith, Legrand (January 2013). "Echinoderms from the Lower Devonian (Emsian) of Bolivia (Malvinokaffric Realm)". Journal of Paleontology. 87 (1): 166–175. doi:10.1666/12-068R.1.
↑Adrain, Jonathan M.; Edgecombe, Gregory D. (1996). "Devonian Aulacopleurid trilobitesof the Malvinokaffric realm". Geobios. 29 (4): 417–436. doi:10.1016/S0016-6995(96)80003-9.
↑Racheboeuf, Patrick R.; Herrera, Zarela (1 September 1994). "On some new Malvinokaffric Silurian and Devonian chonetacean brachiopods, and reclassification of others". Neues Jahrbuch für Geologie und Paläontologie - Monatshefte. 1994 (9): 541–560. doi:10.1127/njgpm/1994/1994/541.
12Babcock, Loren E.; Feldmann, Rodney M.; Wilson, Margaret T.; Suárez-Riglos, Mario (January 1987). "Devonian conulariids of Bolivia". National Geographic Research. 3 (2): 210–231.