2020
DOI: 10.1007/s12549-019-00412-4
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Rodents from Botardo-D and the Miocene-Pliocene transition in the Guadix-Baza Basin (Granada, Spain)

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Cited by 5 publications
(1 citation statement)
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“…1B). The chronostratigraphy of the Baza Formation ranges from the Early Pliocene (Agustí, 1986;Garcés et al, 1996;Piñero and Agustí, 2020) to Middle Pleistocene (Agustí et al, 1987;Agustí et al, 2015b). It is composed of three lithostratigraphic members (Vera et al, 1985;Oms et al, 1998Oms et al, , 2000b: the Lower Member (calcareous surface deposits of a lacustrine and palustrine origin); the Intermediate Member (fluvial mudstones and sandstones); and the Upper Member (lacustrine and palustrine deposits resulting from an accumulation of silty calcareous deposits as well as coarser fractions).…”
Section: J O U R N a L P R E -P R O O Fmentioning
confidence: 99%
“…1B). The chronostratigraphy of the Baza Formation ranges from the Early Pliocene (Agustí, 1986;Garcés et al, 1996;Piñero and Agustí, 2020) to Middle Pleistocene (Agustí et al, 1987;Agustí et al, 2015b). It is composed of three lithostratigraphic members (Vera et al, 1985;Oms et al, 1998Oms et al, , 2000b: the Lower Member (calcareous surface deposits of a lacustrine and palustrine origin); the Intermediate Member (fluvial mudstones and sandstones); and the Upper Member (lacustrine and palustrine deposits resulting from an accumulation of silty calcareous deposits as well as coarser fractions).…”
Section: J O U R N a L P R E -P R O O Fmentioning
confidence: 99%