Also known as Paukkaung kyitchaung 2
Where: Myanmar (21.8° N, 94.7° E: paleocoordinates 13.0° N, 93.1° E)
• coordinate stated in text
• outcrop-level geographic resolution
When: upper Member (Pondaung Formation), Bartonian (41.3 - 38.0 Ma)
• The whole sequence of units was originally defined as the ‘Pondaung Sandstones’ by Cotter (1914), but the horizon yielding Eocene vertebrate fossils is now known as the ‘Upper Member’ of the Pondaung Formation (see Maung et al. 2005). The most recent age for this unit is ~39–38 Ma and so it can be regarded as middle Bartonian (see Tsubamoto et al. 2011).
• formation-level stratigraphic resolution
Environment/lithology: terrestrial; brown, yellow sandstone and red siliciclastic
Size class: macrofossils
Collection methods: this reference only gives a preliminary mention of this fossil, referring the more detailed analysis is in an article which is in press
Primary reference: R. L. Ciochon, P. D. Gingerich, G. F. Gunnell and E. L. Simons. 2001. Primate postcrania from the late middle Eocene of Myanmar. Proceedings of the National Academy of Sciences 98(14):7672-7677 [J. Alroy/E. Leckey/E. Leckey]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 41393: authorized by John Alroy, entered by Erin Leckey on 13.07.2004, edited by K. Christopher Beard, John Alroy, Patricia Holroyd, Takehisa Tsubamoto, Philip Mannion and Grace Varnham
Creative Commons license: CC BY (attribution)
Taxonomic list
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Mammalia | |
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Stenomeryx bahinensis n. gen. n. sp.4
Stenomeryx bahinensis n. gen. n. sp.4 Ducrocq et al. 2020 chevrotain MFP-PK2-2015-1 - holotype; referred material: MFP-PK2-2014-1 and 2015-2
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Paukkaungmeryx minutus n. gen. n. sp.4
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Neochorlakkia myaingensis n. gen. n. sp.3
Neochorlakkia myaingensis n. gen. n. sp.3 Ducrocq et al. 2022 even-toed ungulate Holotype: MFP-PK2-2019-003, isolated right m3
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"cf. Eosimias paukkaungensis" = Bahinia pondaungensis10
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Aseanpithecus myanmarensis n. gen. n. sp.7
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