Reliable systematic identification is a basic premise for paleobiogeographic and paleoecologic analysis. The links between taxonomy and paleobiogeography and paleoecology are evidenced by the necessity to build up ‘objective’ data sets before any analysis in these fields. Reliable taxonomical identifications are only possible by carefully observing the morphology in various diagnostic sections of LBF tests. Routine thin section studies may lead to dramatically incorrect evaluations in the case of non-diagnostic sections of specimens. Furthermore, identification requires specific knowledge and background. In addition to taxa misidentification, another major issue is the lack of a detailed facies analysis, the distribution of foraminifera in these facies units, and their vertical distribution. Without solving all these issues, the interpretations put forward in Sarkar (2019) are mere speculations.

Comment to Sarkar S. (2019) “Does specialization imply rare fossil records of some benthic foraminifera: Late Palaeocene examples from the eastern Neo-Tethys (Meghalaya, NE India)”, Palaeogeogr. Palaeoclimatol. Palaeoecol. 514 (2019) 124–134 / Ozcan, E.; Pignatti, J.. - In: PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY. - ISSN 0031-0182. - 539:(2020). [10.1016/j.palaeo.2019.109528]

Comment to Sarkar S. (2019) “Does specialization imply rare fossil records of some benthic foraminifera: Late Palaeocene examples from the eastern Neo-Tethys (Meghalaya, NE India)”, Palaeogeogr. Palaeoclimatol. Palaeoecol. 514 (2019) 124–134

Pignatti J.
2020

Abstract

Reliable systematic identification is a basic premise for paleobiogeographic and paleoecologic analysis. The links between taxonomy and paleobiogeography and paleoecology are evidenced by the necessity to build up ‘objective’ data sets before any analysis in these fields. Reliable taxonomical identifications are only possible by carefully observing the morphology in various diagnostic sections of LBF tests. Routine thin section studies may lead to dramatically incorrect evaluations in the case of non-diagnostic sections of specimens. Furthermore, identification requires specific knowledge and background. In addition to taxa misidentification, another major issue is the lack of a detailed facies analysis, the distribution of foraminifera in these facies units, and their vertical distribution. Without solving all these issues, the interpretations put forward in Sarkar (2019) are mere speculations.
2020
larger foraminifera; Paleogene; paleobiogeography; paleoecology; Assam; India
01 Pubblicazione su rivista::01b Commento, Erratum, Replica e simili
Comment to Sarkar S. (2019) “Does specialization imply rare fossil records of some benthic foraminifera: Late Palaeocene examples from the eastern Neo-Tethys (Meghalaya, NE India)”, Palaeogeogr. Palaeoclimatol. Palaeoecol. 514 (2019) 124–134 / Ozcan, E.; Pignatti, J.. - In: PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY. - ISSN 0031-0182. - 539:(2020). [10.1016/j.palaeo.2019.109528]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/1363174
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