Herzschuh, Ulrike; Böhmer, Thomas; Li, Chenzhi; Cao, Xianyong; Dolman, Andrew M; Postl, Alexander; Heim, Birgit; Wieczorek, Mareike (2023): Description of sampling sites in the Indopacific region [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.933125
Always quote citation above when using data! You can download the citation in several formats below.
Further details:
Project(s):
Coverage:
Median Latitude: -29.954710 * Median Longitude: 156.353205 * South-bound Latitude: -45.027190 * West-bound Longitude: 107.729050 * North-bound Latitude: -2.540845 * East-bound Longitude: -144.351975
Minimum ELEVATION: 1 m a.s.l. * Maximum ELEVATION: 3910 m a.s.l.
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | Herzschuh, Ulrike | |||
| 2 | Reference/source | Reference | Herzschuh, Ulrike | Event | ||
| 3 | Identification | ID | Herzschuh, Ulrike | Site | ||
| 4 | Identification | ID | Herzschuh, Ulrike | Dataset | ||
| 5 | Site | Site | Herzschuh, Ulrike | |||
| 6 | LONGITUDE | Longitude | Herzschuh, Ulrike | Geocode | ||
| 7 | LATITUDE | Latitude | Herzschuh, Ulrike | Geocode | ||
| 8 | Continent | Cont | Herzschuh, Ulrike | |||
| 9 | ELEVATION | Elevation | m a.s.l. | Herzschuh, Ulrike | Geocode | |
| 10 | Type | Type | Herzschuh, Ulrike | of data | ||
| 11 | Location type | Loc type | Herzschuh, Ulrike | |||
| 12 | Sample amount | N | # | Herzschuh, Ulrike | Pollen samples in core | |
| 13 | Reference/source | Reference | Herzschuh, Ulrike | AgeModel | ||
| 14 | Age, minimum/young | Age min | ka | Herzschuh, Ulrike | ||
| 15 | Age, maximum/old | Age max | ka | Herzschuh, Ulrike | ||
| 16 | Description | Description | Herzschuh, Ulrike | Site Description from Neotoma | ||
| 17 | Reference/source | Reference | Herzschuh, Ulrike | Literature source #1 | ||
| 18 | Uniform resource locator/link to reference | URL ref | Herzschuh, Ulrike | Literature source #1 | ||
| 19 | Reference/source | Reference | Herzschuh, Ulrike | Literature source #2 | ||
| 20 | Uniform resource locator/link to reference | URL ref | Herzschuh, Ulrike | Literature source #2 | ||
| 21 | Reference/source | Reference | Herzschuh, Ulrike | Literature source #3 | ||
| 22 | Uniform resource locator/link to reference | URL ref | Herzschuh, Ulrike | Literature source #3 | ||
| 23 | Reference/source | Reference | Herzschuh, Ulrike | Literature source #4 | ||
| 24 | Uniform resource locator/link to reference | URL ref | Herzschuh, Ulrike | Literature source #4 | ||
| 25 | Reference/source | Reference | Herzschuh, Ulrike | Literature source #5 | ||
| 26 | Uniform resource locator/link to reference | URL ref | Herzschuh, Ulrike | Literature source #5 |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
492 data points
Data
| 1 Event | 2 Reference (Event) | 3 ID (Site) | 4 ID (Dataset) | 5 Site | 6 Longitude | 7 Latitude | 8 Cont | 9 Elevation [m a.s.l.] | 10 Type (of data) | 11 Loc type | 12 N [#] (Pollen samples in core) | 13 Reference (AgeModel) | 14 Age min [ka] | 15 Age max [ka] | 16 Description (Site Description from Neotoma) | 17 Reference (Literature source #1) | 18 URL ref (Literature source #1) | 19 Reference (Literature source #2) | 20 URL ref (Literature source #2) | 21 Reference (Literature source #3) | 22 URL ref (Literature source #3) | 23 Reference (Literature source #4) | 24 URL ref (Literature source #4) | 25 Reference (Literature source #5) | 26 URL ref (Literature source #5) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| BEGASWAM | Neotoma | 247 | 252 | Bega Swamp | 149.500000 | -36.516667 | Indopacific | 1080 | Raw | Swamp | 489 | AWI | -0.045 | 14.487 | NA | Donders, T.H., Haberle, S.G., Hope, G., Wagner, F. and Visscher, H., 2007. Pollen evidence for the transition of the Eastern Australian climate system from the post-glacial to the present-day ENSO mode. Quaternary Science Reviews, 26(11-12), pp.1621-1637. | https://doi.org/10.1016/j.quascirev.2006.11.018 | Hope, G., Kershaw, A.P., van der Kaars, S., Xiangjun, S., Liew, P.M., Heusser, L.E., Takahara, H., McGlone, M., Miyoshi, N. and Moss, P.T., 2004. History of vegetation and habitat change in the Austral-Asian region. Quaternary International, 118, pp.103-126. | https://doi.org/10.1016/S1040-6182(03)00133-2 | Green, D., Singh, G., Polach, H., Moss, D., Banks, J. and Geissler, E.A., 1988. A fine-resolution palaeoecology and palaeoclimatology from south-eastern Australia. Journal of Ecology, 76(3), pp.790-806. | https://doi.org/10.2307/2260574 | Hope, G.S., 1995. Robustness and sensitivity of pollen data-a high resolution record from Bega Swamp. Proceedings of the Climate Change Conference, University of Melbourne and the Australian Quaternary Association, pp.6-8. | Polach, H. and Singh, G., 1980. Contemporary 14C levels and their significance to sedimentary history of Bega Swamp, New South Wales. Radiocarbon, 22(2), pp.398-409. | https://doi.org/10.1017/S0033822200009693 | |
| BLUELAKE | Neotoma | 279 | 285 | Blue Lake | 148.316667 | -36.416667 | Indopacific | 1890 | Raw | Lake | 43 | AWI | 0.216 | 15.333 | Glacial lake 40m deep. Physiography: mountainous. Surrounding vegetation: Alpine heath and scrub. | Raine, J.I. 1974. Pollen sedimentation in relation to Quaternary vegetation history of the Snowy Mountains of New South Wales. Doctoral dissertation. Australian National University, Canberra, Australia. | Raine, J.I., 1982. Dimictic thermal regime and morphology of Blue Lake in the Snowy Mountains of New South Wales. Marine and Freshwater Research, 33(6), pp.1119-1122. | https://doi.org/10.1071/mf9821119 | |||||||
| LGEORGE | Neotoma | 1583 | 1630 | Lake George | 149.429255 | -35.089675 | Indopacific | 673 | Raw | Lake | 66 | AWI | -0.068 | 39.651 | Closed Tectonic basin. Physiography: Hilly, scarp 200m high on western shore. Surrounding vegetation: Eucalypt woodland, grasslands. | Singh, G., Opdyke, N.D. and Bowler, J.M., 1981. Late Cainozoic stratigraphy, palaeomagnetic chronology and vegetational history from Lake George, NSW. Journal of the Geological Society of Australia, 28(3-4), pp.435-452. | https://doi.org/10.1080/00167618108729180 | Singh, G. and Geissler, E.A., 1985. Late Cainozoic history of vegetation, fire, lake levels and climate, at Lake George, New South Wales, Australia. Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences, 311(1151), pp.379-447. | |||||||
| LYNCHA | Neotoma | 1628 | 1683 | Lynch's Crater | 145.686125 | -17.365860 | Indopacific | 760 | Raw | Lake | 234 | AWI | 0.745 | 192.864 | NA | Kershaw, A.P., 1974. A long continuous pollen sequence from north-eastern Australia. Nature, 251(5472), pp.222-223. | https://doi.org/10.1038/251222a0 | Kershaw, A.P., 1976. A late Pleistocene and Holocene pollen diagram from Lynch's Crater, northeastern Queensland, Australia. New Phytologist, 77(2), pp.469-498. | https://doi.org/10.1111/j.1469-8137.1976.tb01534.x | Kershaw, A.P., 1994. Pleistocene vegetation of the humid tropics of northeastern Queensland, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology, 109(2-4), pp.399-412. | https://doi.org/10.1016/0031-0182(94)90188-0 | ||||
| YARLINGT | Neotoma | 2945 | 3043 | Yarlington Tier | 147.300556 | -42.543611 | Indopacific | 650 | Raw | Bog | 21 | AWI | -0.022 | 10.943 | Sphagnum Bog with Beech swamp forest. Physiography: Dolorite Shelf. Surrounding vegetation: Dry Sclerophyll Eucalypt forest. | Harle, K.J., Kershaw, A.P., Macphail, M.K. and Neyland, M.G., 1993. Palaeoecological analysis of an isolated stand of Nothofagus cunninghamii (Hook.) Oerst. in eastern Tasmania. Australian Journal of Ecology, 18(2), pp.161-170. | https://doi.org/10.1111/j.1442-9993.1993.tb00440.x | ||||||||
| KIRKPAT | Neotoma | 9865 | 14622 | Lake Kirkpatrick | 168.573730 | -45.027190 | Indopacific | 570 | Raw | Lake | 26 | AWI | -0.024 | 0.756 | Located in the Lake Wakatipu catchment, southeastern hill country, South Island. Surrounded by pastureland with Agrostis capillaris, Poa spp. and other introduced grasses, Trifolium spp., Hypericum spp., Pinus radiata plantations, and small areas of native Nothofagus menziesii forest. | McWethy, D.B., Wilmshurst, J.M., Whitlock, C., Wood, J.R. and McGlone, M.S., 2014. A high-resolution chronology of rapid forest transitions following Polynesian arrival in New Zealand. PLoS One, 9(11), p.e111328. | https://doi.org/10.1371/journal.pone.0111328 | ||||||||
| DUKES | Neotoma | 9868 | 14629 | Dukes Tarn | 168.492800 | -44.964040 | Indopacific | 830 | Raw | Lake | 46 | Neotoma_McWethy et al. 2014 | 0.003 | 0.792 | Glacial tarn located within the Lake Wakatipu catchment. Surrounding vegetation: patches of trees and shrubs (Nothofagus solandri, Coprosma spp. Phyllocladus, Dracophyllum longifolium, Hebe spp., Gaultheria spp.), native tussock (Chionochloa spp.), and introduced pasture grasses (Festuca spp.). | McWethy, D.B., Whitlock, C., Wilmshurst, J.M., McGlone, M.S., Fromont, M., Li, X., Dieffenbacher-Krall, A., Hobbs, W.O., Fritz, S.C. and Cook, E.R., 2010. Rapid landscape transformation in South Island, New Zealand, following initial Polynesian settlement. Proceedings of the National Academy of Sciences, 107(50), pp.21343-21348. | https://doi.org/10.1073/pnas.1011801107 | McWethy, D.B., Wilmshurst, J.M., Whitlock, C., Wood, J.R. and McGlone, M.S., 2014. A high-resolution chronology of rapid forest transitions following Polynesian arrival in New Zealand. PLoS One, 9(11), p.e111328. | https://doi.org/10.1371/journal.pone.0111328 | ||||||
| BONATOAB | Neotoma | 9979 | 14897 | Bonatoa Bog | 178.533333 | -18.066667 | Indopacific | 4 | Raw | Bog | 21 | AWI | -0.036 | 4.980 | Levee-dammed peatland on delta. Physiography: Estuarine plain, 6 km inland. Regional vegetation: disturbed tropical forest. Local vegetation: Pandanus-sedge-Sphagnum open shrubland. | Hope, G., Stevenson, J. and Southern, W., 2009. Vegetation histories from the Fijian Islands: alternative records of human impact. In: The early prehistory of Fiji. Terra Australis 31. ed. by G. Clark and A. Anderson (pp.63-86). Australian National University Press, Canberra, ACT, Australia. | https://doi.org/10.22459/TA31.12.2009.04 | Hope, G., O'Dea, D. and Southern, W., 1999. Holocene vegetation histories in the Western Pacific: alternative records of human impact. Le Pacifique de 5000 a 2000 avant le present: supplements a l'histoire d'une colonisation ed. by J.C. Galipaud and I. Lilley. Actes du colloque, Vanuatu 31 juillet-6 aout 1996. Collection Colloques et seminaires. Institut de recherche pour le developpement, Paris, France. | Southern, W., 1986. The late Quaternary environmental History of Fiji. Doctoral dissertation. Australian National University, Canberra, Australian Capital Territory, Australia. | ||||||
| BRASS | Neotoma | 9988 | 14921 | Brass Tarn | 145.043180 | -5.787470 | Indopacific | 3910 | Raw | Fen | 49 | AWI | -0.033 | 12.429 | Sedge fen infilling a glacial tarn, perched on wall of deep glacial valley in the Bismarck Range. Located in shrub-rich subalpine grasslands slightly above the tree-line. Local vegetation: Carex gaudichaudiana sedgeland. | Hope, G.S., 1996. History of Nothofagus in New Guinea and New Caledonia. In: The ecology and biogeography of Nothofagus forests ed. by T.T. Veblen, R.S. Hill, and J. Read (pp.257-270). Yale University Press, New Haven, Connecticut, USA. | Hope, G.S. and Peterson, J.A., 1975. Glaciation and vegetation in the high New Guinea mountains. In: Quaternary studies. Bulletin 13 ed. by R.P. Suggate and M.M. Cresswell (pp.155-162). Royal Society of New Zealand, Wellington, New Zealand. | McGlone, M.S., Hope, G., Chappell, J. and Barrett, P., 1996. Past climatic change in Oceania and Antarctica. In: Greenhouse: coping with climate change ed. by J. Bouma, G.I. Pearman, and N.R. Manning (pp.81-99). CSIRO Publishing, Melbourne, Victoria, Australia. | Hope, G.S., 1976. The vegetational history of Mt Wilhelm, Papua New Guinea. The Journal of Ecology, 64(2), pp.627-663. | https://doi.org/10.2307/2258776 | |||||
| IJOMBA | Neotoma | 9996 | 14941 | Ijomba | 137.216945 | -4.020630 | Indopacific | 3630 | Raw | Mire | 32 | Neotoma_Neotoma 1 | -0.031 | 17.159 | Moraine dammed mire in the Discovery Valley on the Kemabu Plateau. Surrounding vegetation: disturbed subalpine forest and treefern. Local vegetation: Astelia hummock bog and Carex fen. | Hope, G.S. and Peterson, J.A., 1975. Glaciation and vegetation in the high New Guinea mountains. In: Quaternary studies. Bulletin 13 ed. by R.P. Suggate and M.M. Cresswell (pp.155-162). Royal Society of New Zealand, Wellington, New Zealand. | Hope, G.S. and Peterson, J.A., 1976. Palaeoenvironments. In: The equatorial glaciers of New Guinea ed. by G.S. Hope, J.A. Peterson, I. Allison, and U. Radok (pp.173-205). A.A. Balkema, Rotterdam, Netherlands. | Flenley, J.R., 1988. Palynological evidence for land use changes in South-East Asia. Journal of Biogeography, 15(1), pp.185-197. | https://doi.org/10.2307/2845059 | Haberle, S.G., Hope, G.S. and van der Kaars, S., 2001. Biomass burning in Indonesia and Papua New Guinea: natural and human induced fire events in the fossil record. Palaeogeography, Palaeoclimatology, Palaeoecology, 171(3-4), pp.259-268. | https://doi.org/10.1016/S0031-0182(01)00248-6 | Hope, G. and Golson, J., 1995. Late Quaternary change in the mountains of New Guinea. Antiquity, 69(265), pp.818-830. | |||
| EAGLTARN | Neotoma | 10004 | 14959 | Eagle Tarn | 146.591200 | -42.679935 | Indopacific | 1033 | Raw | Lake | 55 | AWI | -0.029 | 14.159 | Lake occupies a moraine dammed basin developed by the Broad River glacier during retreat into the Lake Dobson cirque. Surrounding vegetation: Eucalyptus subcrenulata-E. coccifera low open-forest with an understory of Nothofagus cunninghamii; Athrotaxis cuppressoides and Microstrobos niphophilus occurs along creeks and in soaks. | Macphail, M., 1975. The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca. 13,000 - 0 BP). Doctoral dissertation. University of Tasmania, Hobart, Tasmania, Australia. | Macphail, M.K., 1979. Vegetation and climates in southern Tasmania since the last glaciation. Quaternary Research, 11(3), pp.306-341. | https://doi.org/10.1016/0033-5894(79)90078-4 | |||||||
| KOMANLO | Neotoma | 10006 | 14963 | Komanimambuno Mire | 145.089030 | -5.820370 | Indopacific | 2740 | Raw | Mire | 34 | AWI | 1.835 | 34.231 | Abandoned stream meander, steep slopes in upper catchment. Surrounding vegetation: lower montane forest. Local vegetation: Myrtaceous swamp forest. | Hope, G.S. and Peterson, J.A., 1975. Glaciation and vegetation in the high New Guinea mountains. In: Quaternary studies. Bulletin 13 ed. by R.P. Suggate and M.M. Cresswell (pp.155-162). Royal Society of New Zealand, Wellington, New Zealand. | Hope, G.S., 1976. The vegetational history of Mt Wilhelm, Papua New Guinea. The Journal of Ecology, 64(2), pp.627-663. | https://doi.org/10.2307/2258776 | |||||||
| CAMERONS | Neotoma | 10008 | 14969 | Camerons Lagoon | 146.676535 | -41.959050 | Indopacific | 1045 | Raw | Lake | 21 | AWI | -0.035 | 8.909 | Small lake basin of uncertain origin the Central Plateau of Tasmania; fringed by short alpine plant communities and is surrounded on all sides by Liawenee Moor, one of the most extensive treeless expanses in Tasmania. Baumea anhrophylla forms a very open sedgeland in the centre of the lagoon with clear water between it and the banks. Myriophyllum salsugineum, Polomageton sp. and Scirpus sp. grow in patches throughout the lagoon. On poorly drained sites near the margins of the lagoon there are wet heaths of Richea gunnii, Epacris gunnii, Richea sprengelioides and Orites acicularis. The moor is dominated by graminoides, herbs, and shrubs. Well drained, shallow ridges support mat and low heaths. The forests and woodlands that border Liawenee Moor on three sides are dominated by Eucalyptus coccifera, E. gunnii, and E. delegatensis. | Thomas, I. and Hope, G., 1994. An example of Holocene vegetation stability from Camerons Lagoon, a near treeline site on the Central Plateau, Tasmania. Australian Journal of Ecology, 19(2), pp.150-158. | https://doi.org/10.1111/j.1442-9993.1994.tb00478.x | ||||||||
| SUNDOWN | Neotoma | 10009 | 14972 | Sundown Swamp | 144.674630 | -41.126660 | Indopacific | 5 | Raw | Swamp | 13 | AWI | -0.012 | 4.232 | Interdunal Melaleuca ericifolia swamp. Physiography: Coastal plateau with dunes. Surrounding vegetation: Epacris- Leptospermum heath. | Hope, G., 1999. Vegetation and fire response to late Holocene human occupation in island and mainland north west Tasmania. Quaternary International, 59(1), pp.47-60. | https://doi.org/10.1016/S1040-6182(98)00071-8 | ||||||||
| ROTTEN | Neotoma | 10024 | 15005 | Rotten Swamp | 148.886415 | -35.706980 | Indopacific | 1445 | Raw | Swamp | 16 | AWI | -0.068 | 8.036 | Subalpine Sphagnum-Epacris shrub bog with Empodisma fen and Carex fen. Surrounding vegetation: Eucalyptus open forest. | Clark, R.L., 1986. The fire history of Rotten Swamp, A.C.T., Canberra. Unpublished report, ACT Parks and Conservation Service, CSIRO, Canberra, Australia. | Hope, G.S., Nanson, R. and Flett, I., 2009. The peat-forming mires of the Australian Capital Territory. Technical Report 19, Territory and Municipal Services, Canberra, Australian Capital Territory, Australia. | ||||||||
| SUPRIN | Neotoma | 10027 | 15013 | Lac Suprin | 166.991640 | -22.287190 | Indopacific | 235 | Raw | Lake | 33 | AWI | 19.363 | 40.690 | Ephemeral lake in ultramafic karst on Plaine des Lacs, a dissected plateau. Surrounding vegetation: Gymnostoma deplancheanum maquis shrublands. | Hope, G.S., 1996. History of Nothofagus in New Guinea and New Caledonia. In: The ecology and biogeography of Nothofagus forests ed. by T.T. Veblen, R.S. Hill, and J. Read (pp.257-270). Yale University Press, New Haven, Connecticut, USA. | Hope, G. and Pask, J., 1998. Tropical vegetational change in the late Pleistocene of New Caledonia. Palaeogeography, Palaeoclimatology, Palaeoecology, 142(1-2), pp.1-21. | https://doi.org/10.1016/S0031-0182(97)00140-5 | |||||||
| GOG | Neotoma | 10047 | 15059 | Granta Pools | 146.384720 | -41.507870 | Indopacific | 685 | Raw | Lake | 90 | AWI | -0.058 | 7.756 | NA | Fletcher, M.S., Wood, S.W. and Haberle, S.G., 2014. A fire-driven shift from forest to non-forest: evidence for alternative stable states?. Ecology, 95(9), pp.2504-2513. | https://doi.org/10.1890/12-1766.1 | ||||||||
| JACKSONB | Neotoma | 10154 | 15290 | Jacksons Bog | 149.137815 | -37.107945 | Indopacific | 750 | Raw | Bog | 36 | AWI | -0.036 | 15.683 | Valley fen dominated by Carex gaudichaudiana. Physiography: Hilly country. Surrounding vegetation: Eucalyptus obliqua forest and pasture. | Kershaw, A.P., Dunkerley, D.L., Quinn, M. and Southern, W., 1979. A Scientific and environmental investigation of Jackson's Bog, Southern tablelands of N.S.W. Report to National Parks and Wildlife Service of N.S.W. | Oakes, G.M., 1981. The Jacksons Bog peat deposits. GS 1981/596, Geological Survey of New South Wales. | Southern, W., 1982. Late Quaternary vegetation and environments of Jackson's Bog and the Monaro Tablelands, New South Wales. Master's thesis. Monash University, Melbourne, Victoria, Australia. | |||||||
| RR1 | Neotoma | 10526 | 16209 | Ringarooma River | 147.704060 | -41.271550 | Indopacific | 885 | Raw | River | 22 | AWI | -0.039 | 0.878 | The geology of the main peaks and ranges surrounding the river is composed of Devonian granodiorite with small amounts of intrusive metamorphosed Silurian sediments.Temperate rainforest dominates the valley floor. The study sites were located under Nothofagus cunninghamii closed forest, with Leptospermum lanigerttm very prominent in the understorey.Small trees and tall shrubs of P aspleniifoliiis, A. moschatum, Tasmannia lanceolata and T. monganensis, and tree ferns of Dicksonia antarctica are scattered throughout. | Dodson, J.R., Mitchell, F.J.G., Bogeholz, H. and Julian, N., 1998. Dynamics of temperate rainforest from fine resolution pollen analysis, Upper Ringarooma River, northeastern Tasmania. Australian Journal of Ecology, 23(6), pp.550-561. | https://doi.org/10.1111/j.1442-9993.1998.tb00765.x | ||||||||
| TAS1108SC1 | Neotoma | 16395 | 25511 | Lake Vera | 145.880440 | -42.273725 | Indopacific | 571 | Raw | Lake | 116 | AWI | -0.045 | 2.444 | Lake Vera is a moraine-bound lake formed in a glacial valley. It is oligotrophic acidic and dystrophic. Local geology contain siliceous glacial deposits. The steep catchment is Nothofagus-Podocarpaceae cool temperate rainforest and emergent Eucalyptus species overtopping rainforest understory. | Beck, K.K., Fletcher, M.S., Gadd, P.S., Heijnis, H., Saunders, K.M., Simpson, G.L. and Zawadzki, A., 2018. Variance and rate-of-change as early warning signals for a critical transition in an aquatic ecosystem state: a test case from Tasmania, Australia. Journal of Geophysical Research: Biogeosciences, 123(2), pp.495-508. | https://doi.org/10.1002/2017JG004135 | Fletcher, M.S., Benson, A., Bowman, D.M., Gadd, P.S., Heijnis, H., Mariani, M., Saunders, K.M., Wolfe, B.B. and Zawadzki, A., 2018. Centennial-scale trends in the Southern Annular Mode revealed by hemisphere-wide fire and hydroclimatic trends over the past 2400 years. Geology, 46(4), pp.363-366. | https://doi.org/10.1130/G39661.1 | ||||||
| PADDYS | Neotoma | 18866 | 32426 | Paddy's Lake | 145.961595 | -41.451255 | Indopacific | 1065 | Raw | Lake | 184 | AWI | -0.057 | 15.118 | Paddy's Lake is a cirque lake with a maximum depth of 21.5 m. The lake is oligotrophic, acidic and dystrophic. Local geology is Quaternary deposits of quartzite, conglomerate and moraine deposits with traces of Cambrian volcanic conglomerate, sandstone and siltstone. | Beck, K.K., Fletcher, M.S., Gadd, P.S., Heijnis, H. and Jacobsen, G.E., 2017. An early onset of ENSO influence in the extra-tropics of the southwest Pacific inferred from a 14, 600 year high resolution multi-proxy record from Paddy's Lake, northwest Tasmania. Quaternary Science Reviews, 157, pp.164-175. | https://doi.org/10.1016/j.quascirev.2016.12.001 | ||||||||
| DOVE | Neotoma | 19924 | 34553 | Dove Lake | 145.961125 | -41.660615 | Indopacific | 934 | Raw | Lake | 109 | AWI | -0.055 | 11.658 | Lake Dove lies at the northern end of the Cradle Mountain-Lake St. Clair National Park in northwestern Tasmania. | Mariani, M., Connor, S.E., Fletcher, M.S., Theuerkauf, M., Kunes, P., Jacobsen, G., Saunders, K.M. and Zawadzki, A., 2017. How old is the Tasmanian cultural landscape? A test of landscape openness using quantitative land-cover reconstructions. Journal of Biogeography, 44(10), pp.2410-2420. | https://doi.org/10.1111/jbi.13040 | ||||||||
| RAIDA4 | Neotoma | 23920 | 41506 | Ra'irua marsh | -147.678742 | -23.868164 | Indopacific | 1 | Raw | Marsh | 27 | AWI | -0.039 | 1.335 | Ra'irua marsh is a perennial wetland receiving ~2000 mm rainfall annually. The herbaceous vegetation of the marsh is dominated by the introduced herbaceous weeds Ludwigia octovalvis (Jacq.) P.H.Raven, Commelina diffusa Burm.f., Persicaria glabra (Willd.) M.Gomez, and Sagittaria trifolia L. | Prebble, M., Anderson, A.J., Augustinus, P., Emmitt, J., Fallon, S.J., Furey, L.L., Holdaway, S.J., Jorgensen, A., Ladefoged, T.N., Matthews, P.J. and Meyer, J.Y., 2019. Early tropical crop production in marginal subtropical and temperate Polynesia. Proceedings of the National Academy of Sciences, 116(18), pp.8824-8833. | https://doi.org/10.1073/pnas.1821732116 | ||||||||
| EA200 | Neotoma | 23921 | 41514 | Waitetoke | 175.788650 | -36.610150 | Indopacific | 1 | Raw | Swamp | 28 | AWI | -0.057 | 5.509 | Waitetoke swamp on Great Mercury Island is a mostly perennial wetland impounded by a mid-Holocene dune. It is formed within a 10 ha catchment. | Holdaway, S.J., Emmitt, J., Furey, L., Jorgensen, A., O'Regan, R., Phillipps, R., Prebble, M., Wallace, R. and Ladefoged, T.N., 2019. Maori settlement of New Zealand: the Anthropocene as a process. Archaeology in Oceania, 54(1), pp.17-34. | https://doi.org/10.1002/arco.5173 | Prebble, M., Anderson, A.J., Augustinus, P., Emmitt, J., Fallon, S.J., Furey, L.L., Holdaway, S.J., Jorgensen, A., Ladefoged, T.N., Matthews, P.J. and Meyer, J.Y., 2019. Early tropical crop production in marginal subtropical and temperate Polynesia. Proceedings of the National Academy of Sciences, 116(18), pp.8824-8833. | https://doi.org/10.1073/pnas.1821732116 | ||||||
| EA204 | Neotoma | 23922 | 41521 | Tamewhera | 175.759067 | -36.593450 | Indopacific | 17 | Raw | Swamp | 56 | AWI | -0.057 | 0.620 | Tamewhera middle swamp on Great Mercury Island is a perennial wetland. The vegetation of the swamp is dominated by Typha orientalis, but also the rush Juncus ensifolius along with several other herbs, many of which are exotic weeds. Middle swamp positioned below a small upper swamp and a much larger wetland below which is dominated by Typha orientalis. | Prebble, M., Anderson, A.J., Augustinus, P., Emmitt, J., Fallon, S.J., Furey, L.L., Holdaway, S.J., Jorgensen, A., Ladefoged, T.N., Matthews, P.J. and Meyer, J.Y., 2019. Early tropical crop production in marginal subtropical and temperate Polynesia. Proceedings of the National Academy of Sciences, 116(18), pp.8824-8833. | https://doi.org/10.1073/pnas.1821732116 | ||||||||
| TUKOU2 | Neotoma | 23925 | 41532 | Tukou marsh | -144.351975 | -27.604014 | Indopacific | 2 | Raw | Marsh | 30 | AWI | -0.026 | 8.747 | The marsh lies on the south side of the broadest river delta and associated tidal flats at the head of Ha'urei Harbor. The marsh is banked and divided by two smaller prograding river channels forming two waterlogged depressions. The modern marsh appears to have developed behind the southern levee of the main river and the northern levee of the smaller river bounded the marsh to the south. The marsh extends from the estuarine shoreline, marked at high tide (~0.4 m above mean sea level) by driftwood and estuarine detritus, ~135 m to the embankment of the surrounding hill slope. Below the embankment, the marsh reaches a maximum elevation of 3 m above the high tide mark. The topography of the remnant agricultural terrace features lie an additional 50 cm or more above the marsh surface. Tukou is fed by two permanent streams that drain the eastern catchment of Pera'u (650 m a.s.l.), the highest peak on the island. The vegetation of the water-logged marsh surface is currently dominated by introduced pastoral grasses (e.g. Briza minor L.) and adventive herbs (e.g. Calystegia soldanella (L.) R.Br. ex Roem. & Schult. and Commelina diffusa Burm.f.) with some indigenous sedges and rushes. The embankment on the periphery of the marsh has a vegetation cover of grass and naturalized trees. Some indigenous trees are found at the site including Hibiscus tiliaceus L. and Metrosideros collina (J.R Forst. & G.Forst.) A. Gray. | Kennett, D., Anderson, A., Prebble, M., Conte, E. and Southon, J., 2006. Prehistoric human impacts on Rapa, French Polynesia. antiquity, 80(308), pp.340-354. | https://doi.org/10.1017/S0003598X00093662 | Prebble, M., Anderson, A. and Kennett, D.J., 2013. Forest clearance and agricultural expansion on Rapa, Austral archipelago, French Polynesia. The Holocene, 23(2), pp.179-196. | https://doi.org/10.1177/0959683612455551 | Prebble, M., Anderson, A.J., Augustinus, P., Emmitt, J., Fallon, S.J., Furey, L.L., Holdaway, S.J., Jorgensen, A., Ladefoged, T.N., Matthews, P.J. and Meyer, J.Y., 2019. Early tropical crop production in marginal subtropical and temperate Polynesia. Proceedings of the National Academy of Sciences, 116(18), pp.8824-8833. | https://doi.org/10.1073/pnas.1821732116 | ||||
| SWALLOW | Neotoma | 26171 | 45648 | Swallow Lagoon | 153.454722 | -27.498611 | Indopacific | 150 | Raw | Lake | 88 | AWI | -0.053 | 8.119 | Swallow Lagoon (2729'55\ S: 15327'17\ E) is a small (<0.5 ha), perched, freshwater lake that is high in the dunes at ca. 150 m a.s.l. | Mariani, M., Tibby, J., Barr, C., Moss, P., Marshall, J.C. and McGregor, G.B., 2019. Reduced rainfall drives biomass limitation of long-term fire activity in Australia's subtropical sclerophyll forests. Journal of Biogeography, 46(9), pp.1974-1987. | https://doi.org/10.1111/jbi.13628 | ||||||||
| COREDC1 | Neotoma | 19924 | 47110 | Dove Lake | 145.961125 | -41.660615 | Indopacific | 934 | Raw | Lake | 77 | AWI | 0.207 | 17.721 | Lake Dove lies at the northern end of the Cradle Mountain-Lake St. Clair National Park in northwestern Tasmania. | Dyson, W.D., 1994. A pollen and vegetation history from Lake Dove, Western Tasmania. Undergraduate thesis. The University of Newcastle, Callaghan, NSW, Australia. | |||||||||
| TAGIMA10 | Neotoma | 27226 | 48649 | Lake Tagimaucia | -179.939475 | -16.821705 | Indopacific | 823 | Raw | Lake | 61 | AWI | 0.081 | 17.161 | Swamp and open water within the Lake Tagimaucia basin, a volcanic caldera on the east side of Taveuni's main ridge. Vegetation is thick, stunted rainforest (ombrophilous cloud forest) with abundant ferns and mosses. Common trees are Calophyllum vitiense, Macaranga harveyana, Geniostoma vitiense, Dysoxylum sp., Rapanea myricifolia, Palaquium hornei, Podocarpus neriifolius, and Neubergia alata, also treeferns Cyathea alta and C. medullaris and palms Veitchia simulans and Clinostigma exorrhiza. | Hope, G., Stevenson, J. and Southern, W., 2009. Vegetation histories from the Fijian Islands: alternative records of human impact. In: The Early Prehistory of Fiji ed by G. Clark and A. Anderson (pp.63-86). Australian National University Press, Canberra. | https://doi.org/10.22459/TA31.12.2009.04 | Southern, W., 1986. The late Quaternary environmental History of Fiji. Doctoral dissertation. Australian National University, Canberra, Australian Capital Territory, Australia. | |||||||
| NADRAU | Neotoma | 27228 | 48653 | Nadrau Swamp | 177.958440 | -17.711120 | Indopacific | 760 | Raw | Peat | 31 | AWI | -0.036 | 2.553 | Site is a sedge fen. Upland vegetation is forest with Endospermum macrophyllum, Parinari insularurn, Agathis vitiensis, Dacrdium nidulum, Podocarpus neriifolius, Palaquium sp., Dysoxylum richii, Calophyllum spp., and species of Myrtaceae. A stand of Erythrinia sp., presumably planted, occurs on the eastern margin of the swamp. The western margin has low forest of Decaspermum vitiense, Aglaia elegans, Podocarpus neriifolius, Garcinia pseudoguttifera, and Dacrycarpus imbricatus. The wetland vegetation is severely disturbed by cattle grazing with a high proportion of introduced taxa, including sedges Cyperus pilosus, Kyllinga brevifolia, and Rhynchospora corymbosa and the grass Paspalum conjugatum. | Hope, G., Stevenson, J. and Southern, W., 2009. Vegetation histories from the Fijian Islands: alternative records of human impact. In: The Early Prehistory of Fiji ed by G. Clark and A. Anderson (pp.63-86). Australian National University Press, Canberra. | https://doi.org/10.22459/TA31.12.2009.04 | Hope, G., O'Dea, D. and Southern, W., 1999. Holocene vegetation histories in the Western Pacific: alternative records of human impact. In: Le Pacifique de 5000 a 2000 avant le present: supplements a l'histoire d'une colonisation ed by J.-C. Galipaud and I. Lilley (pp.387-404). Institut de recherche pour le developpement, Paris. | Southern, W., 1986. The late Quaternary environmental History of Fiji. Doctoral dissertation. Australian National University, Canberra, Australian Capital Territory, Australia. | ||||||
| HORDORLI | Neotoma | 27229 | 48656 | Lake Hordorli | 140.589915 | -2.540845 | Indopacific | 798 | Raw | Lake | 60 | AWI | 0.059 | 53.267 | Closed solution basin in ltramafics. Physiography: Flat area mid-slope. Surrounding vegetation: Lower montane forest with gynosperms Araucaria cunninghamii, Papuacedrus papuana, Phyllocladus hypophyllus and Podocarpus spp. Microphyll-leafed angiosperm taxa dominate, such as Cryptocarya, Litsea, Dysoxylum, Galbulimima belgraveana, Garcinia graminea, Planchonella cyclopensis, Timonius, Ardisia and Stenocarpus moorei. Dipterocarps such as Hopea sp. and the oaks, for example, Lithocarpus molluccana, occur occasionally, together with a wide array of Moraceae and Myrtaceae. The surface vegetation on the lake consists of an open sedgeland ~40 cm in height, which is often flooded for short periods. | Hope, G., 2015. Extended vegetation histories from ultramafic karst depressions. Australian Journal of Botany, 63(4), pp.222-233. | https://doi.org/10.1071/BT14283 | Hope, G. and Tulip, J., 1994. A long vegetation history from lowland Irian Jaya, Indonesia. Palaeogeography, Palaeoclimatology, Palaeoecology, 109(2-4), pp.385-398. | https://doi.org/10.2307/2845439 | ||||||
| BANDUNG2 | Neotoma | 27233 | 48666 | Bandung DPDR-II | 107.729050 | -6.990417 | Indopacific | 662 | Raw | Lake | 100 | AWI | 4.931 | 121.972 | Intermontane basin with former lake. Physiography: Plain between volcanos. Surrounding vegetation: Secondary forest disturbed by urban development. Local vegetation: Grassland. | Dam, M.A.C., 1994. The late Quaternary evolution of the Bandung Basin, West-Java, Indonesia. Doctoral dissertation. Vrije Universiteit Amsterdam, Amsterdam, The Netherlands. | Van Der Kaars, S. and Dam, R., 1997. Vegetation and climate change in West-Java, Indonesia during the last 135,000 years. Quaternary International, 37, pp.67-71. | https://doi.org/10.1016/1040-6182(96)00002-X | Van der Kaars, W.A. and Dam, M.A.C., 1995. A 135,000-year record of vegetational and climatic change from the Bandung area, West-Java, Indonesia. Palaeogeography, Palaeoclimatology, Palaeoecology, 117(1-2), pp.55-72. | https://doi.org/10.1016/0031-0182(94)00121-N |