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- W1996707796 abstract "Morphological, stratigraphical, micropaleontological and radiocarbon dating investigations of the gravelly Kaitorete “Spit” system, Canterbury, New Zealand show that a barrier/spit system has existed at this site for the last 8000 yr. Kaitorete “Spit” developed as a true spit extending north from near the Rakaia river mouth, during sea level rise in the Late Pleistocene and Early Holocene. This produced an estuarine coastline along the southwestern flank of Banks Peninsula. The spit extended to Banks Peninsula sometime in the early mid-Holocene creating a barrier lake complex behind the spit. Since the mid-Holocene, there have been at least three fluctuations between lacustrine and estuarine/lagoonal conditions in the barrier blocked system. The most recent fluctuation, which resulted in the present barrier lake complex, occurred within the last 200–500 yr. These fluctuations are associated with the avulsion of a large braided river, the Waimakariri, to and from the Lake Ellesmere basin. When the river flows through the basin, a permanent channel is maintained to the ocean with estuarine conditions present. When the river flows elsewhere, the barrier closes and a freshwater lake system forms behind it. This study emphasises the importance of fluvial control on the evolution of gravelly coastlines where sediment supply is not the limiting factor. Both the sediments and the water in the back barrier area are predominantly derived from the terrestrial catchment. We highlight the absence of true marine influence in the back barrier area, except in the vicinity of the tidal channel, even when such a channel is present. Marine processes have been limited to the gradual re-orientation of the barrier system from drift to swash alignment." @default.
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- W1996707796 date "1997-04-01" @default.
- W1996707796 modified "2023-09-26" @default.
- W1996707796 title "The Holocene evolution of a well nourished gravelly barrier and lagoon complex, Kaitorete “Spit”, Canterbury, New Zealand" @default.
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- W1996707796 doi "https://doi.org/10.1016/s0025-3227(97)00003-0" @default.
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