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- W2073647597 abstract "This study clearly indicates that pollen grains and certain other maceration-resistant microfossils found in surface sediment of the Great Bahama Bank are sedimented primarily in response to water turbulence and other hydrological factors. Low levels of pine-pollen concentration are found in the same areas as sandy sediment—areas of relatively turbulent water. Muddy sediment and high levels of pine-pollen concentration are similarly associated in the areas of sluggish water movement. This is very significantly true of the area of quiet water west of Eleuthera Island, where pine pollen occurs abundantly in the mud, despite the absence of pine trees on the island. This shows that pine pollen is moved about widely on the Bank and sediments out in the areas of relatively nonturbulent water. The discovery that large amounts of pine pollen—as much as 2,000 per 100 l. of water—are present in the water on the Bank months after the trees ceased flowering further substantiates this fact. “Microforaminifera” are more generally distributed; they occur both in muddy sediment and in sandy sediment at various locations. Apparently they are found more or less where they lived, having been moved about relatively little on the Bank. Hystrichosphaerids show a distribution intermediate between that of pine pollen and that of “microforaminifera”; they are relatively concentrated in the muddy sediment, as a response to nonturbulence of the water, but they also sediment out to some extent at other locations on the Bank. This is interpreted as showing that hystrichosphaerids are denser than pine pollen. The study shows the possible use of palynological analysis in the investigation of paleosediment types and paleohydrologic features of sedimentary basins." @default.
- W2073647597 created "2016-06-24" @default.
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- W2073647597 date "1967-08-01" @default.
- W2073647597 modified "2023-10-16" @default.
- W2073647597 title "Pollen and associated microfossils in the marine surface sediments of the Great Bahama Bank" @default.
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- W2073647597 doi "https://doi.org/10.1016/0034-6667(67)90057-7" @default.
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