Wanganui Basin

The Wanganui Basin (also spelled Whanganui Basin) is an onshore-offshore basin on the North Island of New Zealand. The basin provides an important stratigraphic and palaeontological record for the late Neogene marine environment of New Zealand.[1][2][3]

Cliff at Kai Iwi Beach

Location and setting

The Wanganui Basin is located on the west coast of the North Island of New Zealand, within the Manawatū-Whanganui and Taranaki regions. The basin is roughly oval in shape, with the longer (approximately 180 kilometres (110 mi)) axis running west-south-west/east-north-east, and has a width of approximately 100 kilometres (62 mi). A little under half of the basin is onshore, extending inland around the lower reaches of the Whanganui and Rangitikei Rivers before terminating at the foot of the North Island Volcanic Plateau. The southern half of the basin extends into the South Taranaki Bight. The major population centre within the basin is along the coast, around the city of Whanganui.

Geology

Stratigraphy
Main article: New Zealand geologic time scale

The Wanganui Basin is "one of the most complete late Neogene marine stratigraphic records in the world,"[1] and is an important region for geological and palaeontological research.[2][3]

The basin provides the basis for the eponymous Wanganui epoch in the New Zealand geologic time scale, which covers the Pliocene, Pleistocene and Holocene over the last 5.33 million years.[1][4] The series was first described in depth and compared to glacial cycles by Charles Fleming,[3][5] which has had a lasting impact upon subsequent stratigraphic, palaeontological and palaeoecological research.[2] Each stage within the Wanganui epoch is named after regions of the Wanganui Basin series.[4]

Key sites
Kai Iwi Beach
  • Castlecliff
  • Nukumaru

Palaeontology

Sediments within the basin are rich with shallow marine invertebrate fossils, including molluscs[5] and bryozoans.[6] The most common fossilized molluscan shells belong to the bivalve genera Dosinia and Chlamys and the gastropod genera Zethalia and Murex.[3] Shells of Aeneator, Buccinulum, Penion, Alcithoe, and Amalda marine snails are also frequent.[5]

gollark: https://git.osmarks.tk/osmarks/potatOS#architecture
gollark: Are you NOT horrifyingly aware of the complexity of the PotatOS architecture?
gollark: Of course!
gollark: It's actually enforced, see.
gollark: PotatoBIOS.

See also

References
  1. Carter, Robert M.; Naish, Tim R. (1998). "A review of Wanganui Basin, New Zealand: global reference section for shallow marine, Plio–Pleistocene (2.5–0 Ma) cyclostratigraphy". Sedimentary Geology. 122 (1–4): 37–52. doi:10.1016/S0037-0738(98)00097-9.
  2. Crampton, James S. M.; Cooper, Roger A. (2010). "The state of paleontology in New Zealand". Palaeontologia Electronica. 13 (1). ISSN 1094-8074.
  3. "Dr Alan Beu". www.sciencelearn.org.nz. 18 May 2011. Retrieved 23 July 2019.
  4. Beu, Alan G. (2001). "Local stages to be used for the Wanganui Series (Pliocene-Pleistocene), and their means of definition". New Zealand Journal of Geology and Geophysics. 44 (1): 113–125. doi:10.1080/00288306.2001.9514928.
  5. Beu, Alan G.; Maxwell, P.A. (1990). Cenozoic Mollusca of New Zealand. New Zealand Geological Survey Bulletin. 58. Lower Hutt, New Zealand: New Zealand Department of Scientific and Industrial Research. ISSN 0114-2283.
  6. Rust, S.; Gordon, D. (2011). "Plio-Pleistocene Bryozoan faunas of the Wanganui Basin, New Zealand: stratigraphic distribution and diversity". New Zealand Journal of Geology and Geophysics. 54 (2): 151–165. doi:10.1080/00288306.2010.514928.

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.