Interpreting pollen diagrams from wetlands: pollen representation in surface samples from Oil Well Bog, southern Ontario

1998 ◽  
Vol 76 (10) ◽  
pp. 1780-1797 ◽  
Author(s):  
M Jane Bunting ◽  
Barry G Warner ◽  
Clayton R Morgan

Pollen and spore analysis of surface sediment samples from 45 points within Oil Well Bog, a coniferous swamp near Cambridge, Ontario, was used to determine the possibility of identifying different wetland vegetation communities from their palynological record, and to assess the effects of variable wetland vegetation on the pollen representation of surrounding upland communities. The data obtained were mapped for individual taxa to allow direct comparison of the spatial patterns of vegetation abundance and the associated palynological assemblages, and cluster analysis was used to identify palynologically similar assemblages. Some wetland communities, such as swamp dominated by black spruce, do have distinctive pollen signatures, but not all the vegetational diversity observed is reflected in the palynological data, with similar pollen assemblages deriving from some communities which are vegetationally very different (e.g., shrub swamps dominated by Chamaedaphne calyculata and Ilex verticillata). The wetland pollen assemblages do reflect much of the floristic diversity of the surrounding uplands, although the different communities receive varying proportions of their pollen influx from upland sources (varying from less than 5% to over 90%), and wide variations in the percentage of a given upland pollen morphotype can be found within quite a short distance, depending on the nature of local wetland communities.Key words: palynology, swamp, surface samples, wetland.

1998 ◽  
Vol 76 (10) ◽  
pp. 1770-1779 ◽  
Author(s):  
M Jane Bunting ◽  
Clayton R Morgan ◽  
Mark Van Bakel ◽  
Barry G Warner

A vegetation survey at Oil Well Bog, southern Ontario, suggested that the central Picea mariana - Sphagnum (black spruce swamp) community represented the most mature point in the wetland succession. Pollen analysis of short sediment cores from beneath three major communities in the wetland (black spruce swamp, white pine swamp, and low shrub swamp) showed that the black spruce community only became established in the last 100 years. From around 2000 BP, the wetland was dominated by low shrubs with a tall shrub element. Upland forest composition around the wetland changed around 500 BP, with a decrease in percentages of Fagus and an increase in Pinaceae. At the same time trees colonized parts of the wetland. When the upland forest was cleared by European settlers (ca. AD 1830-1845), low shrub communities reestablished, suggesting that initially the wetland surface became wetter. Over time, the present-day mosaic of swamp types began to develop. The pollen analyses showed that the black spruce swamp is present as a result of changes in the wetland hydrology induced by human activity, and the fragmentary low shrub vegetation community (which contains locally rare plant species) represents a relic of the pre-European settlement wetland community.Key words: paleoecology, wetland development, hydroseral succession.


For the period ca. 15000-10000 years ago, which spans the interval between the latest presence of lowland ice and the final disappearance of mountain glaciers from Britain, so many botanical data are now available that it is possible to analyse plant distributions and vegetation composition in detail not yet possible for earlier periods. Species lists, provided by identification of pollen and of macroscopic remains, show a combination of diverse phytogeographic elements into an assemblage characteristic of the period - an admixture of apparently thermophilous plants with those now found in northern and arctic situations, and of oceanic and steppe elements. Ordination of data on floras has revealed much similarity between the regions of Britain, but pollen analysis continues to emphasize how strong must have been the regional differentiation of vegetation. A comparison of pollen diagrams published since 1970, from sites lying on a broad north-south transect of western Britain, shows much variety in the pollen assemblage zones which have been distinguished, and in the vegetation interpreted from the pollen data by comparison with surface samples and modern vegetation. Sufficient 14C dating is now available, however, to permit chronostratigraphic correlation of these pollen zones, and to show that there is consistent evidence for climatic amelioration at about 13000 B.P., and rapid deterioration at about 11000 B.P., leading to conditions of incomplete vegetation cover and universal soil disturbance which can be correlated with geomorphological evidence for the recrudescence of mountain glaciation in western Scotland, the Lake District, and North Wales, in the period called Younger Dryas on the continental mainland. Between 13000 and 11000 there is in western Britain evidence for a woodland biozone, or palaeobotanical interstadial, equivalent to Bolling plus Allerod of continental stratigraphers (Mangerud, Andersen, Berglund & Donner 1974), and divided by a very minor regression of vegetation during Older Dryas time ( ca. 12000-11800). The now closely 14 C-dated site at Low Wray Bay, Windermere, is described in detail, and suggested as a reference site for this interstadial.


1988 ◽  
Vol 64 (4) ◽  
pp. 345-351 ◽  
Author(s):  
R. D. Whitney

Armillaria root rot. caused most likely by Armillaria obscura (Pers) Herink, killed 6-to 21-year-old white spruce, black spruce, jack pine and red pine saplings in each of 49 plantations examined in northern Ontario. Annual mortality in the four species over the last 2 to 6 years averaged 1.4%, 1.5%, 0.5% and 0.2%, respectively. In all but one of 25 white spruce and red pine plantations (43 to 58 years old) in eastern and southern Ontario. Armillaria root rot was associated with mortality. Accumulated mortality in white spruce and red pine (initially recorded in 1978) averaged 7.6% and 11.7%, respectively, as of 1986. Current annual mortality for all plantations ranged from 0% to 16%. Key words: root rot. Armillaria obscura, white spruce, black spruce, jack pine, red pine.


1970 ◽  
Vol 14 ◽  
pp. 59-66
Author(s):  
Khum Narayan Paudayal

Palynological investigation of ten samples obtained from a drill core belonging to the Late Pleistocene deposits of the PatanFormation in the Kathmandu Valley revealed 40 plant species belonging to 22 families. The gymnosperms are represented byAbies, Picea, Pinus spp. (P. roxburghii and P. wallichiana) and Tsuga sp. The angiosperm tree and shrubs are represented bygenera Quercus (Q. semecarpifolia, Q. lanata, Q. leucotricophora and Q. lamellosa and Q. glauca), Castanopsis, Alnus, Betula,Carpinus, Juglans, Myrica, Ulmus, Ilex, Strobilanthes, Elaeagnus and families Meliaceae, Oleaceae, Ericaceae, Poaceae,Compositae, Caryophyllaceae, Chenopodiaceae, Apiaceae, and Dipsacaceae. Similarly the wetland and aquatic plants arerepresented by Polygonun, Myriophyllum and Trapa. The presence of significant number of pteridophytes indicates humid anddamp environment at the periphery of the lake and surrounding forest floor. The pollen assemblage suggests that the PatanFormation was deposited under humid subtropical climate except at the middle part which indicates of warm temperate climaticcondition. The result obtained from the recent surface samples analysis and its comparison with fossil assemblages show thatmodern pollen spectra are not different with the fossil assemblages. This justifies that the fossil palynomorphs are local and itdenies the influence of exotic pollen.DOI: http://dx.doi.org/10.3126/bdg.v14i0.5440Bulletin of the Department of Geology Vol.14 2011, pp.59-66 


1993 ◽  
Vol 71 (2) ◽  
pp. 193-210 ◽  
Author(s):  
George A. King

The relationship between the vegetation and modern pollen assemblages in eastern Canada is summarized and analyzed using isopoll maps, ordination, and cluster analysis. The major vegetation zones are shrub tundra, forest tundra (divided into shrub and forest subzones), lichen woodland, closed black spruce forest, mixed boreal forest, and coastal barrens. The pollen assemblages of these zones are distinguished by differences in the relative abundance of a few important pollen types rather than by floristic differences. Northern zones have relatively high Cyperaceae and low Picea pollen percentages, and southern zones have high Picea and Abies pollen percentages. Surface samples from each vegetation zone generally form distinctive groups in the ordination analysis. However, samples from the shrub subzone of the forest tundra cluster with shrub tundra samples, and lichen woodland samples cluster with samples from the closed black spruce forest and the forest subzone of the forest tundra. Cluster analysis separates the samples into geographically distinct groups. However, these groups generally contain samples from several vegetation zones. The surface sample data set analyzed here will prove useful in reconstructing the vegetation history of the region. Key words: pollen surface samples, modern vegetation, eastern Canada.


1990 ◽  
Vol 80 (3) ◽  
pp. 365-370 ◽  
Author(s):  
Terence J. Blake ◽  
Weixing Tan ◽  
Suzanne R. Abrams

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