Shanwang Bed sw4, Linchu district, Shantung province: Burdigalian, China
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Amphibia
- Temnospondyli
- Bufonidae
|
||||||||||
Bufo linquensis n. sp.
Yang 1977
|
Yang 1977 | |||||||||
part/counterpart of a nearly complete specimen | ||||||||||
Mammalia
- Chiroptera
- Vespertilionidae
|
||||||||||
Shanwangia unexpectata n. gen., n. sp.
Yang 1977
|
Yang 1977 | |||||||||
multiple specimens, at least one nearly complete with part/counterpart | ||||||||||
Mammalia
- Soricidae
|
||||||||||
Lusorex taishanensis n. gen., n. sp.
Storch and Qiu 2004
|
Storch and Qiu 2004 | |||||||||
Mammalia
|
||||||||||
Palaeochoerus cf. pascoei
|
||||||||||
Mammalia
- Perissodactyla
- Rhinocerotidae
|
||||||||||
Brachypotherium shanwangensis
(Wang 1965)
|
||||||||||
recombined as Diaceratherium shanwangensis | ||||||||||
see common names |
Geography
Country: | China | State/province: | Shandong |
Coordinates: | 36.5° North, 118.5° East (view map) | ||
Paleocoordinates: | 36.4° North, 116.1° East | ||
Basis of coordinate: | based on nearby landmark |
Time
Period: | Neogene | Epoch: | Miocene |
Stage: | Burdigalian | 10 m.y. bin: | Cenozoic 5 |
Key time interval: | Burdigalian | ||
Age range of interval: | 20.44000 - 15.98000 m.y. ago |
Stratigraphy
Formation: | Shanwang | Member: | Upper | ||
Local order: | bottom to top | ||||
Stratigraphy comments: MN6, Aragonian, Middle Miocene. There are six layers, which are grouped into 3 members. These members contain 3 fossil-bearing beds. The greatest exposure of SW4 is on Xiao Yao Hill (18m) and is thinnest (a lens 1m deep) on Jiao Yan Hill. Fossils found on Xiao Yao Hill.
From He et al. 2011: "40Ar/39Ar ages obtained from basalts of the Niushan and Yaoshan Formations, which underlie and overlie the Shanwang Formation, are 21.0 ± 2.5 Ma (2σ, full external error) and 17.3 ± 1.5 Ma (2σ, full external error), respectively. The 40Ar/39Ar age of the basalt in the Shanwang Formation is 17–18 Ma. Given the age constraints of the basalts of the Yaoshan and Shanwang Formations, the age of the Shanwang biota is estimated to be ca. 17 Ma, late Burdigalian of the Early Miocene,". Yu et al. 2021 support this, stating "Paleomagnetic and radio isotope dating data shows that the diatomaceous shale was deposited during Chron C5En, which places it at approximately 18.5 Ma during the Burdigalian stage of the Early Miocene, rather than in the Middle Miocene as previously thought." |
Lithology and environment
Primary lithology: | conglomerate |
Secondary lithology: | mudstone |
Lithology description: 'Yellowsih brown basaltic sandy conglomerate intercalated with arenaceous mud stone.' | |
Environment: | lacustrine indet. |
Taphonomy
Modes of preservation: | body,adpression |
Size of fossils: | macrofossils |
Articulated whole bodies: | some |
Collection methods and comments
Reason for describing collection: | biostratigraphic analysis |
Collection method comments: Flora indicates 'climate in the coastal region of China was then more humid and one of sub-tropical belt, while central parts of the continent were comparatively drier.'
| |
Taxonomic list comments:The fauna needs revising. The following species are listed by Qiu, but he does not state which member they are from: Ansomys shanwangensis (aplodontid), Plesiosciurus aff. sinensis (sciurid), Hemicyon (Phoberocyon) youngi, Ursavus orientalis, Thaumastocyoninae indet., Probsicidea indet., Brachypotherium sp., Chalicotherium grande, Palaeomeryx tricornis, Lagomeryx spp., Suinae. |
Metadata
Database number: | 43397 | ||
Authorizer: | A. Turner, L. van den Hoek Ostende, D. Smith | Enterer: | H. O'Regan, E. Leckey, L. van den Hoek Ostende |
Modifier: | G. Varnham | Research group: | PACED |
Created: | 2004-08-13 07:10:02 | Last modified: | 2022-05-06 04:26:38 |
Access level: | the public | Released: | 2004-08-13 07:10:02 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
11442. | PACED | D. Yan, Z. Qiu, and Z. Meng. 1983. Miocene Stratigraphy and mammals of Shanwang, Shandong. Vertebrata PalAsiatica 21(3):210-222 [A. Turner/H. O'Regan/H. O'Regan] |
Secondary references:
11208 | PACED | Z. Qiu. 1990. The Chinese Neogene mammalian biochronology - its correlation with the European Neogene mammal zonation. In E.H. Lindsay, V. Fahlbusch and P. Mein, eds., European Neogene Mammal Chronology. Plenum Press, New York. 527-556 [A. Turner/H. O'Regan/H. O'Regan] |
25658 | G. Storch and Z. Qiu. 2004. First complete heterosoricine shrew: A new genus and species from the Miocene of China. Acta Palaeontologica Polonica 49(3):357-363 [L. van den Hoek Ostende/L. van den Hoek Ostende] | |
15140 | J. Yang. 1977. On some Salientia and Chiroptera from Shanwang, Linqu, Shandong. Vertebrata Palasiatica 15(1):76-80 [D. Smith/E. Leckey] |