Late quaternary pollen stratigraphy, geology and soils of an area near Greytown : a thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Soil Science at Massey University

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dc.contributor.authorTompkins, Joanna Olive
dc.date.accessioned2017-05-08T22:26:03Z
dc.date.available2017-05-08T22:26:03Z
dc.date.issued1987
dc.description.abstractIn the southern Wairarapa Valley there are extensive gravel fans, built by the Tauherenikau, Waiohine, and Waingawa Rivers. The fans form the Waiohine Surface which is lapped by a complex of Holocene fluvial, lacustrine and estuarine deposits. At the toe of the fans, peat deposits have accumulated over early Holocene sediments. This study involved; a) detailed mapping of the Quaternary deposits and soils and, b) analysis of pollen stratigraphy from continuous peat deposits in an area south of Greytown, in order to establish the Late Quaternary vegetative and environmental changes in the area. Detailed mapping showed that the c. 6,000 years B.P. Holocene high sea level did not encroach the area as was previously believed. After the formation of the Waiohine Surface c.10,000 years B.P., the Waiohine and possibly Tauherenikau Rivers infilled the area with aggradational gravels and sands. At c.8,500 years B.P. these river systems left the area and, peat deposits began accumulating soon after. The pollen spectrum, dated from c.8,500 years B.P. at the base, to c.5,500 years B.P. at the surface showed that the vegetation in the area suffered little change during the period of peat accumulation. Substantial areas of shrub, herbaceous and swamp communities existed in the valley, in addition to a Dacrydium cupressinum dominated podocarp-hardwood forest. Stands of Dacrycarpus dacrydioides were prominent on many wetter sites. A podocarp-hardwood complex, with areas of Nothofagus existed in the adjacent ranges. Climatic deterioration may have caused the rise in Nothofagus at the expense of the podocarps after 6,000 years B.P. The steady decline of D. dacrydioides with respect to D. cupressinum between 6,000 years B.P. and 5,000 years B.P. however, is a result of local drying around the bog. Fluctuations in vegetation are not of sufficient magnitude to justify the use of pollen zones.en_US
dc.identifier.urihttp://hdl.handle.net/10179/10868
dc.language.isoenen_US
dc.publisherMassey Universityen_US
dc.rightsThe Authoren_US
dc.subjectNew Zealanden_US
dc.subjectWairarapaen_US
dc.subjectGeologyen_US
dc.subjectStratigraphicen_US
dc.subjectQuaternaryen_US
dc.titleLate quaternary pollen stratigraphy, geology and soils of an area near Greytown : a thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Soil Science at Massey Universityen_US
dc.typeThesisen_US
massey.contributor.authorTompkins, Joanna Oliveen_US
thesis.degree.disciplineSoil Scienceen_US
thesis.degree.grantorMassey Universityen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Science (M. Sc.)en_US
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