O'Connell, Michael; Molloy, Karen (2018): Pollen profile SHE IV, Lough Sheeauns, Connemara, Co. Galway [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.896818, In: O'Connell, M; Molloy, K (2018): Lough Sheeauns, Connemara, Co. Galway (profile SHE IV): exploratory investigations of peat deposit from near the lake margin [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.896820
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2018-12-18 • DOI registered: 2019-01-16
Related to:
Keane, Sinéad (1989): Palaeoecological studies at Lough Sheeauns, Cleggan, Co. Galway [thesis]. B.Sc. (Hons) thesis, Department of Botany, University College Galway (NUIG)
Molloy, Karen; O'Connell, Michael (1991): Palaeoecological investigations towards the reconstruction of woodland and land-use history at Lough Sheeauns, Connemara, western Ireland. Review of Palaeobotany and Palynology, 67, 75-113
Coverage:
Latitude: 53.557100 * Longitude: -10.074680
Minimum DEPTH, sediment/rock: 0.64 m * Maximum DEPTH, sediment/rock: 2.58 m
Event(s):
SHE_IV (Lough Sheeauns) * Latitude: 53.557100 * Longitude: -10.074680 * Elevation: 25.0 m * Recovery: 3 m * Method/Device: Livingstone corer (LIVC) * Comment: This peat core was taken 33 m to the east of L. Sheeauns. Exploratory pollen analytical investigations only were carried out in the context of an undergraduate project (Keane 1989). Geology: Mainly schist. On a geological divide; fertile soils to north; less fertile to south where there is a thin covering of blanket bog is widespread. Archaeology: High concentration of megaliths (tombs and a standing stone alignment). Basin size: Core SHE IV taken near the southern side of the outflow channel (drain; this has been deepened), 33 m to the east of the lake edge. Sampling in field: Top m using a gouge corer; sampled to 310 cm using 5 cm diameter Livingstone corer in 1 m drives. Depth of data collection: 1987 (best estimate). Stratigraphy: peat (partly woody) with silt at base. Length of core: 64-258 m. Spans from ca. AD 500 to early Holocene (short LG sequence in final drive, i.e. 5-6 m; not analysed).
Parameter(s):
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
968 data points
Data
| 1 Depth sed [m] | 2 Comment | 3 Pin [#] | 4 Que [#] | 5 Ulm [#] | 6 Aln [#] | 7 Cor/Myr [#] | 8 Bet [#] | 9 Sal [#] | 10 Frx [#] | 11 Ile [#] | 12 Hed [#] | 13 Lon [#] | 14 Sor [#] | 15 Mon.f.s [#] | 16 Ppd.v [#] | 17 Ptd [#] | 18 Osmu [#] | 19 Poac [#] | 20 Pla.l [#] | 21 Pti-T [#] | 22 Ran-T [#] | 23 Rum-T [#] | 24 Suc [#] | 25 Tri.r [#] | 26 Vic-T [#] | 27 Fabae [#] | 28 Flp [#] | 29 Mel [#] | 30 Hyp [#] | 31 Cypae [#] | 32 Cal [#] | 33 Vac-T [#] | 34 Nat [#] | 35 Clh [#] | 36 Mey.t [#] | 37 Pollen corroded [#] | 38 Sph [#] | 39 Charcoal [#] | 40 Til.s [#] | 41 Gel [#] | 42 Samp vol [cm3] | 43 Lyc(ad) [#] | 44 Lyc(ct) [#] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.64 | 1 | 2 | <1 | 5 | 15 | 24 | 4 | <1 | 0 | 3 | 0 | 1 | 2 | 0 | 4 | 1 | 24 | 2 | 9 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 128 | 1 | 0 | 1 | 0 | 5 | 3 | 8 | 0 | 2 | 1 | 16500 | 23 | |
| 0.80 | 1 | 24 | 0 | 9 | 18 | 147 | 5 | 0 | 1 | 1 | 0 | 1 | 2 | 0 | 1 | 0 | 44 | 1 | 7 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 5 | 1 | 0 | 0 | 0 | 7 | 10 | 20 | 0 | 17 | 1 | 16500 | 23 | |
| 1.04 | 2 | 26 | 1 | 15 | 45 | 149 | 0 | 0 | 3 | 2 | 0 | 3 | 124 | 1 | 3 | 0 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 1 | 16500 | 3 | |
| 1.12 | 4 | 29 | 2 | 52 | 80 | 139 | 0 | 0 | 1 | 10 | 0 | 0 | 3 | 9 | 0 | 0 | 4 | 0 | 0 | 9 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 4 | 0 | 33 | 0 | 2 | 1 | 16500 | 11 | |
| 1.20 | Pinus has declined (ca. 3000 BP); human activity registers | 7 | 12 | 2 | 39 | 51 | 30 | 4 | 0 | 0 | 1 | 0 | 2 | 16 | 5 | 23 | 1 | 98 | 45 | 29 | 12 | 1 | 0 | 5 | 0 | 4 | 0 | 0 | 0 | 9 | 11 | 0 | 1 | 0 | 0 | 1 | 69 | 1 | 0 | 0 | 1 | 16500 | 27 |
| 1.28 | 24 | 74 | 7 | 65 | 60 | 32 | 1 | 0 | 9 | 5 | 3 | 1 | 26 | 24 | 6 | 1 | 4 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 7 | 0 | 3 | 0 | 0 | 1 | 16500 | 46 | |
| 1.36 | 33 | 147 | 10 | 67 | 46 | 37 | 1 | 0 | 7 | 5 | 0 | 3 | 14 | 8 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 1 | 16500 | 15 | |
| 1.44 | 82 | 41 | 8 | 66 | 43 | 29 | 1 | 0 | 0 | 3 | 1 | 2 | 4 | 1 | 2 | 0 | 56 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 12 | 0 | 0 | 1 | 16500 | 24 | |
| 1.51 | 8 | 25 | 3 | 66 | 34 | 22 | 2 | 0 | 0 | 3 | 0 | 5 | 8 | 12 | 0 | 0 | 37 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 13 | 0 | 4 | 1 | 16500 | 5 | |
| 1.60 | Rise in Alnus (begin Atlantic period) | 28 | 9 | 2 | 84 | 41 | 66 | 3 | 0 | 0 | 5 | 0 | 8 | 25 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 9 | 0 | 0 | 0 | 0 | 1 | 16500 | 1 |
| 1.68 | 97 | 10 | 6 | 3 | 18 | 49 | 1 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 5 | 0 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 26 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 16500 | 17 | |
| 1.75 | 51 | 14 | 1 | 0 | 27 | 5 | 1 | 0 | 0 | 9 | 0 | 1 | 1 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 4 | 0 | 0 | 0 | 0 | 3 | 4 | 0 | 0 | 0 | 1 | 16500 | 13 | |
| 1.84 | 17 | 14 | 2 | 0 | 68 | 106 | 4 | 0 | 0 | 5 | 0 | 0 | 2 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 0 | 1 | 1 | 16500 | 1 | |
| 1.90 | 37 | 24 | 8 | 1 | 128 | 50 | 8 | 0 | 0 | 2 | 1 | 0 | 12 | 22 | 7 | 0 | 8 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 4 | 0 | 122 | 1 | 0 | 0 | 0 | 0 | 3 | 1 | 21 | 0 | <1 | 1 | 16500 | 37 | |
| 2.00 | 4 | 25 | 4 | 0 | 27 | 135 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 17 | 4 | 0 | 0 | 1 | 16500 | 19 | |
| 2.08 | 74 | 36 | 2 | 1 | 83 | 40 | 1 | 0 | 0 | 0 | 0 | 5 | 2 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 1 | 16500 | 7 | |
| 2.16 | 83 | 22 | 0 | 0 | 46 | 24 | 4 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 25 | 0 | 0 | 0 | 0 | 0 | 4 | 4 | 8 | 0 | 0 | 1 | 16500 | 28 | |
| 2.24 | 16 | 16 | 8 | 1 | 57 | 20 | 33 | 0 | 0 | 0 | 1 | 0 | 1 | 12 | 4 | 1 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 2 | 0 | 51 | 3 | 0 | 0 | 0 | 0 | 21 | 3 | 5 | 1 | 0 | 1 | 16500 | 67 | |
| 2.32 | 4 | 5 | 3 | 0 | 39 | 51 | 25 | 0 | 0 | 0 | 0 | 2 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 0 | 7 | 10 | 0 | 0 | 0 | 0 | 0 | 34 | 17 | 9 | 0 | 1 | 16500 | 37 | |
| 2.40 | 8 | 17 | 0 | 0 | 50 | 34 | 25 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 49 | 0 | 10 | 21 | 0 | 0 | 0 | 0 | 0 | 37 | 7 | 39 | 0 | 1 | 16500 | 31 | |
| 2.47 | 5 | 8 | 6 | 0 | 61 | 29 | 5 | 0 | 0 | 1 | 2 | 2 | 0 | 1 | 0 | 13 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 3 | 60 | 0 | 0 | 0 | 3 | 0 | 19 | 1 | 8 | 0 | 1 | 16500 | 21 | |
| 2.50 | 6 | 4 | 1 | 0 | 72 | 83 | 3 | 0 | 0 | 1 | 0 | 1 | 3 | 1 | 0 | 3 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 4 | 4 | 0 | 0 | 0 | 2 | 2 | 76 | 1 | 10 | 0 | 1 | 16500 | 44 | |
| 2.58 | 33 | 4 | 3 | 0 | 54 | 27 | 6 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 1 | 18 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 2 | 0 | 0 | 0 | 2 | 10 | 2 | 0 | 0 | 0 | 1 | 16500 | 45 |
