2004
DOI: 10.1016/s1040-6182(03)00066-1
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The indicative meaning of diatoms, pollen and botanical macro fossils for the reconstruction of palaeoenvironments and sea-level fluctuations along the coast of Lower Saxony; Germany

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Cited by 40 publications
(36 citation statements)
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“…These include the Beaufort Sea (Campeau et al 2000), the western Belgian coast (Denys 1989), the western coastline of the United States and Canada , the Lower Saxony, Germany (Freund et al 2004), and the coastal plains of Japan (Kumano et al 1990). In some of these studies, diatom dissolution terra australis 32 occurred to the extent that full counts of each sample could not always be obtained Denys 1989;.…”
Section: Resultsmentioning
confidence: 99%
“…These include the Beaufort Sea (Campeau et al 2000), the western Belgian coast (Denys 1989), the western coastline of the United States and Canada , the Lower Saxony, Germany (Freund et al 2004), and the coastal plains of Japan (Kumano et al 1990). In some of these studies, diatom dissolution terra australis 32 occurred to the extent that full counts of each sample could not always be obtained Denys 1989;.…”
Section: Resultsmentioning
confidence: 99%
“…However, pollen is still extremely useful as it is the only microfossil, which provides climate or chrono-horizon information in addition to an indicative meaning. As Freund et al (2004) highlight, the use of pollen in sea-level reconstructions in temperate regions is hindered by the rather coarse resolution of the assemblages. One example is Plantago maritima, which is indicative of a low marsh environment but due to its ubiquitous pollen dispersal, is found throughout the marsh environment.…”
Section: Pollen As a Proxy Indicator Of Past Sea-levelmentioning
confidence: 99%
“…Early sea-level research relied heavily on the use of marsh pollen as a proxy for sea-level, with the first sea-level curve produced by God win ( 1940) in the English fenland. Developments within the last 30 years in the use of the vertical zonations of foraminifera (Scott and Medioli, 1978) and diatoms (Zong 1997) have resulted in a movement away from pollen as a sealevel proxy in the last ten years, partly due to the coarse resolution of pollen assemblages (Freund et al, 2004) and its apparent unsuitability as a quantitative approach to sea-level reconstruction. Work by Horton et al (2005a) and Debenay et al (2004) have shown that Foraminifera are capable of reconstructing sea level in tropical environments, however the fossil record is prone to preservation issues with Debenay et al (2004) stating that foraminifera in mangrove environments are "dramatically affected by taphonomic processes".…”
Section: Introductionmentioning
confidence: 99%
“…In coastal peatlands, the changing interface between the marine and terrestrial landscape strongly influences peatland water levels and water quality (Freund et al 2004). Diatoms are regarded as very sensitive indicators of changes in water quality (Stoermer and Smol 1999) and are useful tools to describe palaeoenvironmental conditions in humiferous as well as in clastic lithofacies, such as those that accumulate in coastal lagoons.…”
Section: Introductionmentioning
confidence: 99%
“…These include the Beaufort Sea (Campeau et al 2000), the western Belgian coast (Denys 1989), the western coastline of the United States and Canada (Eronen et al 1987), the Lower Saxony, Germany (Freund et al 2004), and the coastal plains of Japan (Kumano et al 1990). In some of these studies, diatom dissolution terra australis 32 occurred to the extent that full counts of each sample could not always be obtained (Eronen et al 1987;Denys 1989;Campeau et al 2000).…”
Section: Introductionmentioning
confidence: 99%