O'Connell, Michael (2018): Age determination at Lough Doo, Co. Mayo, Ireland [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.892444, In: O'Connell, M (2018): Holocene environmental reconstruction at Lough Doo, Co. Mayo, Ireland: pollen, chemistry and palaeomagnetics [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.892447
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2018-07-16 • DOI registered: 2018-08-14
Related to:
O'Connell, Michael (1990): Early land use in north-east County Mayo - the palaeoecological evidence. Proceedings of the Royal Irish Academy, 90C, 259-279, http://www.jstor.org/stable/25516069
O'Connell, Michael; Mitchell, Fraser J G; Readman, P W; Doherty, T J; Murray, Declan A (1987): Palaeoecological investigations towards the reconstruction of the post-glacial environment at Lough Doo, County Mayo, Ireland. Journal of Quaternary Science, 2(2), 149-164, https://doi.org/10.1002/jqs.3390020208
Further details:
Coverage:
Latitude: 54.050210 * Longitude: -9.096010
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 2.880 m
Event(s):
LOUGHDOO (Lough Doo, DOO) * Latitude: 54.050210 * Longitude: -9.096010 * Elevation: 20.0 m * Lake water depth: 8 m * Method/Device: Mackereth corer (MACC) * Comment: EPD: Local vegetation: Fraximus, Salix, Sorbus, Crataegus, Prunus. Location: centre of lake. O'Connel Data: Lough Doo, Co. Mayo (700 m east of Attymass). 3 m Mackereth corer (pneumatic corer provided by Dr Alan Hamilton, Uni of Ulster (Coleraine); see Mackereth (1958). Max. depth, ca. 13 m, towards eastern side of lake. Core taken in ca. 8 cm of water close to middle of lake. Date of lake coring: 1981 (summer).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Age, dated material | Dated material | O'Connell, Michael | |||
| 2 | Laboratory code/label | Lab label | O'Connell, Michael | 14C Lab No | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | O'Connell, Michael | Geocode – Depths cited in m, with respect to the top of core (uppermost - most recent sediment probably not retrieved). | |
| 4 | Depth, top/min | Depth top | m | O'Connell, Michael | ||
| 5 | Depth, bottom/max | Depth bot | m | O'Connell, Michael | ||
| 6 | Age, dated | Age dated | ka | O'Connell, Michael | Age, 14C AMS | |
| 7 | Age, dated, standard deviation | Age dated std dev | ± | O'Connell, Michael | Age, 14C AMS | |
| 8 | Laboratory code/label | Lab label | O'Connell, Michael | Galway Lab No | ||
| 9 | Age, comment | Comm | O'Connell, Michael | |||
| 10 | Thickness | Thick | cm | O'Connell, Michael |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
73 data points
Data
| 1 Dated material | 2 Lab label (14C Lab No) | 3 Depth sed [m] (Depths cited in m, with respe...) | 4 Depth top [m] | 5 Depth bot [m] | 6 Age dated [ka] | 7 Age dated std dev [±] | 8 Lab label (Galway Lab No) | 9 Comm | 10 Thick [cm] |
|---|---|---|---|---|---|---|---|---|---|
| Top of core | Based on pollen | 0.000 | Top of core; uppermost sediment not recovered. Pollen suggests that the top of core probably relates to early 19C | 1 | |||||
| Bulk gyttja sample | GrN-11739B | 0.620 | 0.59 | 0.65 | 2.800 | 0.10 | DOO 4b | Age reversal due to erosion of peaty soils from catchment | 6 |
| Bulk gyttja sample | GrN-11739 | 0.725 | 0.65 | 0.80 | 2.510 | 0.05 | DOO 4a | Age reversal due to erosion of peaty soils from catchment | 15 |
| Bulk gyttja sample | GrN-11738B | 1.665 | 1.64 | 1.69 | 1.510 | 0.12 | DOO 3b | 5 | |
| Bulk gyttja sample | GrN-11738 | 1.775 | 1.69 | 1.86 | 1.895 | 0.05 | DOO 3a | 17 | |
| Bulk gyttja sample | GrN-11737 | 2.260 | 2.21 | 2.31 | 4.610 | 0.06 | DOO 2a | 10 | |
| Bulk gyttja sample | GrN-11737B | 2.340 | 2.31 | 2.37 | 5.020 | 0.23 | DOO 2b | 6 | |
| Bulk gyttja sample | GrN-11736 | 2.770 | 2.73 | 2.81 | 6.280 | 0.07 | DOO 1a | 8 | |
| Bulk gyttja sample | GrN-11736B | 2.835 | 2.81 | 2.86 | 6.750 | 0.21 | DOO 1b | 5 | |
| Base of core (bottom on non-consolidated sediment not reached) | Based on pollen | 2.880 | Base of core; Late-glacial/Early Holocene transition not reached |