1949
DOI: 10.1017/s0025315400055284
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The Fauna of Sand and Mud Banks Near the Mouth of the Exe Estuary

Abstract: Erosion of Dawlish Warren, at the mouth of the Exe Estuary has resulted in a redistribution of sand, which has come to lie in close proximity to certain of the original mud banks.Quantitative collections of the macrofauna were made along a traverse passing from the newly deposited sand to the old mud bank, stations all being at about half-tide level.Measurements of salinity, temperature, pH, currents and wave action show that these are similar for all stations. Thus it has been possible to observe the distribu… Show more

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Cited by 80 publications
(41 citation statements)
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“…All the major species are well-known representatives of the Macoma community, except for Ampharete which is not usually associated with this assemblage elsewhere and appears to be peculiar to south-west England. It is common in regions of higher salinity in the Tamar (Spooner & Moore, 1940) and Exe (Holme, 1949). The dominance of the errant polychaete Nephtys hombergi rather than Nereis diversicolor is typical of the Macoma community at the higher end of its salinity range.…”
Section: Species Compositionmentioning
confidence: 99%
“…All the major species are well-known representatives of the Macoma community, except for Ampharete which is not usually associated with this assemblage elsewhere and appears to be peculiar to south-west England. It is common in regions of higher salinity in the Tamar (Spooner & Moore, 1940) and Exe (Holme, 1949). The dominance of the errant polychaete Nephtys hombergi rather than Nereis diversicolor is typical of the Macoma community at the higher end of its salinity range.…”
Section: Species Compositionmentioning
confidence: 99%
“…A descriptive account of the estuary has been given by Holme (1949), to which little can be added. Four transects along the eastern shore were selected for quantitative sampling, two across the muddy shores at Topsham (To) and Lympstone (Ly), and two across the sands at Shelly Bank (Sh) and Orcombe Point (Op) level could not be sampled.…”
Section: Description Of Study Areamentioning
confidence: 99%
“…Synthesizing existing data on communities from the North Sea, Jones (1950) placed "communities" and "zones" into specific sediment types, noting that differences in the supply of detritus and organism mobility might contribute to observed patterns. Still, when Thorson (1957) synthesized the available data on infaunal distributions, developing the concept of "parallel levelbottom communities", very few studies actually included quantitative information on the sediments (e.g., grain-size distributions) in which the organisms were collected (some exceptions include, for example, Ford, 1923;Sparck, 1933;Stephen, 1933;Thorson & Ussing, 1934;Holme, 1949). In fact, it was the dual effect of Thorson's (1957) generalisations and Sanders ' (1958) observation that different infaunal feeding types tended to dominate sandy versus muddy sediments that prompted the plethora of -subsequent studies of the relationship between distributions of infauna and sediments (e.g., Table 1).…”
Section: Infauna and Sediments Historical Perspectivementioning
confidence: 99%