Grant, Michael J (2018): Lithology of sediment core CRANESMO, Cranes Moor, United Kingdom [dataset]. European Pollen Database (EPD), PANGAEA, https://doi.org/10.1594/PANGAEA.888035
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Published: 2018-04-06 • DOI registered: 2018-06-05
Related to:
Grant, Michael J; Hughes, P D M; Barber, K E (2009): 13. Early to mid-Holocene vegetation-fire interactions and responses to climatic change at Cranes Moor, New Forest. In: R.M. Briant, M.R. Bates, R.T. Hosfield, and F.F. Wenban-Smith (Eds). The Quaternary of the Solent Basin and West Sussex raised beaches. Quaternary Research Association, London, 198 - 214
Grant, Michael J; Hughes, P D M; Barber, K E (2014): Climatic influence upon early to mid-Holocene fire regimes within temperate woodlands: a multi-proxy reconstruction from the New Forest, southern England. Journal of Quaternary Science, 29(2), 175-188, https://doi.org/10.1002/jqs.2692
Coverage:
Latitude: 50.827770 * Longitude: -1.725830
Minimum DEPTH, sediment/rock: 0.225 m * Maximum DEPTH, sediment/rock: 0.755 m
Event(s):
CRANESMO (Cranes Moor) * Latitude: 50.827770 * Longitude: -1.725830 * Elevation: 45.0 m * Method/Device: Russian corer (RUSC) * Comment: Mire. Physiography: plateau. Surrounding vegetation: cultivated field and forest. Local vegetation: wet heath and Sphagnum lawn. Location: 1 km west of Burley village. Notes: in area of Mesolithic occupation. Core diameter: 9 cm. Additional device: Monolith tin
Comment:
This dataset was archived on 2018-04-04 from the EPD database (http://www.europeanpollendatabase.net).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Grant, Michael J | Geocode | |
| 2 | Depth, top/min | Depth top | m | Grant, Michael J | of the lithological unit | |
| 3 | Depth, bottom/max | Depth bot | m | Grant, Michael J | of the lithological unit | |
| 4 | Lithology/composition/facies | Lithology | Grant, Michael J |
License:
(UNKNOWN)
Size:
12 data points