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Revista mexicana de ciencias geológicas
versión On-line ISSN 2007-2902versión impresa ISSN 1026-8774
Resumen
ARENILLAS, Ignacio y ARZ, José Antonio. Origin and evolution of the planktic foraminiferal Family Eoglobigerinidae Blow, 1979, during the early Danian (Paleocene). Rev. mex. cienc. geol [online]. 2013, vol.30, n.1, pp.159-177. ISSN 2007-2902.
New evidence on the origin and diversification of the plankticforaminiferal Family Eoglobigerinidae Blow, 1979, or Paleocene spinose, cancellate lineage, has been discovered from some of the most continuous lower Danian sections known to date, especially from El Kef and Aïn Settara (Tunisia). Based on the discovery of transitional specimens, we suggest an evolution from primitive, smooth walled Palaeoglobigerina Arenillas, Arz and Náñez, 2007, to cancellate Eoglobigerina Morozova, 1959, and then on to Parasubbotina Olsson, Hemleben, Berggren and Liu, 1992, and Subbotina Brotzen and Pozaryska, 1961. The transition from Palaeoglobigerina to Eoglobigerina implied progressive textural changes in the wall surface, such as the development of pore-pits, spines and eventually a cancellate wall. This transition, however, implied minor external morphologic changes between ancestral Palaeoglobigerina fodina (Blow, 1979) and its descendant Eoglobigerina simplicissima (Blow, 1979), such as the increase in test size and the thickness of the apertural lip.
Palabras llave : Paleocene; wall texture; spinose; eoglobigerinid; phylogeny.