Moar, Neville T (2010): Lithology of sediment core MOSSCREE, Moss of Cree, United Kingdom [dataset]. European Pollen Database (EPD), PANGAEA, https://doi.org/10.1594/PANGAEA.741569
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Lewis, Francis John (1906): The plant remains in the Scottish peat Mosses - I. The Scottish Southern Uplands. Transactions of the Royal Society of Edinburgh, 41(3), 699-723, https://doi.org/10.1017/S0080456800035559
Moar, Neville T (1969): Late Weichselian and Flandrian pollen diagrams from southwest Scotland. New Phytologist, 68(2), 433-467, http://www.jstor.org/stable/2431362
Coverage:
Latitude: 54.923333 * Longitude: -4.450000
Minimum DEPTH, sediment/rock: 0.3000 m * Maximum DEPTH, sediment/rock: 6.0000 m
Event(s):
Comment:
This dataset was archived on 2010-05-11 from the EPD database.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, top/min | Depth top | m | Moar, Neville T | of the lithological unit | |
| 3 | Depth, bottom/max | Depth bot | m | Moar, Neville T | of the lithological unit | |
| 4 | Lithology/composition/facies | Lithology | Moar, Neville T |
License:
Creative Commons Attribution-NonCommercial 3.0 Unported (CC-BY-NC-3.0)
Size:
30 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Lithology |
|---|---|---|---|
| 0.3000 | 0.0000 | 0.6000 | Not sampled |
| 0.7250 | 0.6000 | 0.8500 | Brown humified Sphagnum peat |
| 0.9750 | 0.8500 | 1.1000 | Dark humified Sphagnum peat |
| 1.5000 | 1.1000 | 1.9000 | Dark humified Sphagnum peat |
| 2.2000 | 1.9000 | 2.5000 | Dark humified Sphagnum peat |
| 3.1000 | 2.5000 | 3.7000 | Sphagnum peat with macrofossils |
| 3.9000 | 3.7000 | 4.1000 | Silty clay containing wood fragments |
| 4.5500 | 4.1000 | 5.0000 | Blue-grey clay with minute plant remains |
| 5.5000 | 5.0000 | 6.0000 | Stiff blue-grey clay |
| 6.0000 | 6.0000 | 6.0000 | Not sampled |