Brassington Formation
Stratigraphic range: Mid-Late Miocene Serravallian-Tortonian
TypeGeological formation
Unit ofGreat Britain Superficial Deposits Supergroup
Sub-unitsKirkham Member, Bees Nest Member, Kenslow Member
UnderliesAlluvium
OverliesCarboniferous Limestone (Peak Limestone Group)
AreaStaffordshire, Derbyshire
Thicknessup to 70 metres (230 ft)
Lithology
PrimarySand
OtherClay, Silt, Gravel
Location
RegionEurope
Country UK
Extent220 km2
Type section
Named forBrassington
Named byBoulter et al.
LocationBees' Nest Pit
Year defined1971
Thickness at type section43 metres (140 ft)

The Brassington Formation is a geological formation in the United Kingdom, and the country's most significant onshore Miocene deposit. it is preserved as around 60 inliers in karsts of Carboniferous limestone, specifically the Peak Limestone Group, in a triangular region on the borders of the Staffordshire and Derbyshire counties. The lithology largely consists of unconsolidated sand with clay and minor silt components. Pebble beds are also a significant component. It is divided up into three members, which are in ascending order the Kirkham Member, Bees Nest Member and the Kenslow Member. The Kenslow Member is dated to the Serravallian to Tortonian stages based on palynology.

Lithology

The main source rocks for the Brassington Formation are the Triassic sandstones of the Sherwood Sandstone Group.[1]

Kirkham Member

The Lithology of the Kirkham member consists of up to 40–50 m of cream or white coloured (originally red coloured) kaolinitic fluvial derived unfossiliferous sand, gravel and pebble beds, possibly with local cementation.

Bees Nest Member

The lithology of the Bees Nest Member consists of interbedded mottled sandy and silty clays of varying colours (green, grey, red and yellow brown), it is 6 m thick in the Bees Nest pit and up to 21 m in the Kenslow Pit. It represents a low energy aquatic or lacustrine depositional setting

Kenslow Member

The Lithology of the Kenslow Member consists of up to 6 m of massive lacustrine grey coloured clay, with the uppermost parts containing abundant wood fragments preserved as mummifications.[2] It was deposited in a shallow lacustrine to swampy setting.[3] Some outcrops of the Kenslow Member have lignite lenses.[2]

Paleoenvironmental interpretation

The vegetation from the Kenslow member suggests a subtropical, seasonally wet climate, with a temperature range of 23.6-28.3°C for the warmest month, and 1.8-12.5°C for the coldest month.[4] [5] The palynomorph assemblage is dominated by pollen of the genera Picea, Pinus, Tsuga and Sciadopitys, the last of which today is confined to a single species in Japan. It was probably deposited close to sea level, but a significant distance from the sea. Fossil wood and pollen referable to the genus Cryptomeria has also been found.[4] Fossil fungi have also been reported from the Kenslow Member.[6]

References

  1. ^ Walsh, Peter T.; Banks, Vanessa J.; Jones, Peter F.; Pound, Matthew J.; Riding, James B. (2018-01-31). "A reassessment of the Brassington Formation (Miocene) of Derbyshire, UK and a review of related hypogene karst suffosion processes". Journal of the Geological Society. 175 (3): 443–463. doi:10.1144/jgs2017-029. ISSN 0016-7649. S2CID 135442239.
  2. ^ a b O'Keefe, Jennifer M.K.; Pound, Matthew J.; Riding, James B.; Vane, Christopher H. (March 2020). "Cellular preservation and maceral development in lignite and wood from the Brassington Formation (Miocene), Derbyshire, UK" (PDF). International Journal of Coal Geology. 222: 103452. doi:10.1016/j.coal.2020.103452. S2CID 216281365.
  3. ^ Pound, Matthew J.; Riding, James B.; Donders, Timme H.; Daskova, Jirina (June 2012). "The palynostratigraphy of the Brassington Formation (Upper Miocene) of the southern Pennines, central England". Palynology. 36 (1): 26–37. doi:10.1080/01916122.2011.643066. S2CID 129857989.
  4. ^ a b Pound, Matthew J.; Riding, James B. (2015-11-10). "Palaeoenvironment, palaeoclimate and age of the Brassington Formation (Miocene) of Derbyshire, UK" (PDF). Journal of the Geological Society. 173 (2): 306–319. doi:10.1144/jgs2015-050. ISSN 0016-7649. S2CID 53550587.
  5. ^ McCoy, Jessica; Barrass-Barker, Tabitha; Hocking, Emma P.; O'Keefe, Jennifer M.K.; Riding, James B.; Pound, Matthew J. (1 October 2022). "Middle Miocene (Serravallian) wetland development on the northwest edge of Europe based on palynological analysis of the uppermost Brassington Formation of Derbyshire, United Kingdom" (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology. 603: 111180. doi:10.1016/j.palaeo.2022.111180. S2CID 251432511.
  6. ^ Pound, Matthew J.; O’Keefe, Jennifer M. K.; Nuñez Otaño, Noelia B.; Riding, James B. (5 December 2018). "Three new Miocene fungal palynomorphs from the Brassington Formation, Derbyshire, UK" (PDF). Palynology. 43 (4): 596–607. doi:10.1080/01916122.2018.1473300. S2CID 134737967.
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