Harami 4
Basic information
Sample name: Harami 4
Reference: P. Joniak, P. Pelaez-Campomanes, S. Mayda, M. Bilgin, K. Halaclar, and L. W. van den Hoek Ostende. 2019. New faunas of small mammals from old Harami mine (early Miocene, Anatolia, Turkey). Palaeobiodiversity and Palaeoenvironments 99:673-700 [ER 3900]
Geography
Country: Turkey
State: Central Anatolia
Coordinate: 38.45435° N, 31.82708° E
Coordinate basis: estimated from map
Formation: Harmanyazi Formation
Time interval: Early Miocene
Zone: MN2
Max Ma: 22.268
Min Ma: 21.992001
Age basis: other
Geography comments: Harami 4 is located in the Harami lignite mine in Ilgın, NW of Konya, Central Anatolia
Through faunal comparisons and integrated stratigraphy, Harami 4 has been equated with Harami 1, which was dated through palaeomagnetism to Chron 6Bn.2n (22.268–21.992 Ma)
Through faunal comparisons and integrated stratigraphy, Harami 4 has been equated with Harami 1, which was dated through palaeomagnetism to Chron 6Bn.2n (22.268–21.992 Ma)
Environment
Lithology: lignite
Taphonomic context: lake deposit
Habitat comments: Harami is part of the Ilgın Basin, an intra-montane basin consisting of "continental clastic sediments unconformably resting on a basement of Palaeozoic metamorphics and Mesozoic limestones"
Harami 4 is situated in the Harmanyazi Member (Graben) of the Ilgın Formation, an Early Miocene formation composed of "claystone, marl, limestone, and coal interbeds"
"The lignite seams in Ilgın region occurs at the base of the lacustrine sequence of the Harmanyazi Formation which mainly consists of whitish marls up to 180 m thick"
Harami 4 is located "within the lignites"
The presence of beavers and the diversity of insectivores indicate a "swamp forest with a lush undergrowth"
Harami 4 is situated in the Harmanyazi Member (Graben) of the Ilgın Formation, an Early Miocene formation composed of "claystone, marl, limestone, and coal interbeds"
"The lignite seams in Ilgın region occurs at the base of the lacustrine sequence of the Harmanyazi Formation which mainly consists of whitish marls up to 180 m thick"
Harami 4 is located "within the lignites"
The presence of beavers and the diversity of insectivores indicate a "swamp forest with a lush undergrowth"
Methods
Life forms: rodents,other small mammals
Sampling methods: quarry
Sample size: 217 specimens
Years: 2015
Sampling comments: Specimen counts are recovered from systematic palaeontology material
Roughly 500 kg of sediment was recovered from Harami 4
Specimens are primarily teeth
Roughly 500 kg of sediment was recovered from Harami 4
Specimens are primarily teeth
Metadata
Sample number: 4289
Contributor: Jack Nesbitt
Enterer: Jack Nesbitt
Created: 2023-05-31 12:51:42
Modified: 2023-09-11 10:53:28
Abundance distribution
18 species
2 singletons
total count 217
geometric series index: 26.2
Fisher's α: 4.661
geometric series k: 0.7883
Hurlbert's PIE: 0.8345
Shannon's H: 2.1649
Good's u: 0.9909
Each square represents a species. Square sizes are proportional to counts.
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Register
| Galerix saratji | 10 | |
| Theratiskos rutgeri | 9 | |
| Suleimania ruemkae | 4 | |
| Desmanodon ziegleri | 4 | |
| Turkodimylus hartogi | 2 | |
| Dinosorex anatolicus | 7 | |
| Glirudinus haramiensis | 6 | |
| Glirudinus cf. matusi | 3 | |
| Bransatoglis complicatus | 2 | |
| Vasseuromys cf. duplex | 3 | |
| Mirrabella anatolica | 1 | |
| Eumyarion microps | 42 | |
| Eumyarion carbonicus | 57 | |
| Eumyarion sp. nov. | 47 | |
| "Eumyarion n. sp." | ||
| Deperetomys intermedius | 3 | |
| Democricetodon anatolicus | 14 | |
| Sciuridae indet. | 1 | |
| "Sciuridae gen. et sp. indet." | ||
| Steneofiber eseri | 2 | |