2006
DOI: 10.1016/j.palaeo.2005.12.016
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Oncoids from the river Alz (southern Germany): Tiny ecosystems in a phosphorus-limited environment

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Cited by 77 publications
(37 citation statements)
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“…In fact, it has been suggested that one of the main reasons why there are living microbialites in this region is because stoichiometric nutrient constraints prevent snails and potentially other eukaryotes from effectively grazing the microbialites (Elser et al ., 2005a). Oncolites similar to those found in Cuatro Ciénegas are also actively forming in the German river Alz, where phosphorus levels are extremely low (Hagele et al ., 2006). In Rio Mesquites, phosphorus enrichment experiments have demonstrated significant increases in primary production and biogenic calcification, along with major decreases in biomass C:P and N:P ratios in oncolites after P enrichment (Elser et al ., 2005b).…”
Section: Resultsmentioning
confidence: 99%
“…In fact, it has been suggested that one of the main reasons why there are living microbialites in this region is because stoichiometric nutrient constraints prevent snails and potentially other eukaryotes from effectively grazing the microbialites (Elser et al ., 2005a). Oncolites similar to those found in Cuatro Ciénegas are also actively forming in the German river Alz, where phosphorus levels are extremely low (Hagele et al ., 2006). In Rio Mesquites, phosphorus enrichment experiments have demonstrated significant increases in primary production and biogenic calcification, along with major decreases in biomass C:P and N:P ratios in oncolites after P enrichment (Elser et al ., 2005b).…”
Section: Resultsmentioning
confidence: 99%
“…6B). Comparable oncoids have been reported and described in detail from other rivers and lakes of the Molasse Basin (Schäfer & Stapf 1978, Rott 1991, Hägele et al 2006. Locally, tufa stromatolites cover the stream bottom, which is considered by some ecologists to have a negative impact on the distribution of the highly endangered noble crayfish (Astacus astacus) which still occurs in this region (Schütze in Peršoh 1998).…”
Section: Descriptionmentioning
confidence: 87%
“…With regard to their spherical morphology and concentric growth pattern, movement and rotation of the tufa oncoids does not seem to be a crucial prerequisite (Hägele et al 2006). Nonetheless, occasional flooding events shift and rotate the oncoids in the river Moosach, and cause temporary decline in calcite supersaturation.…”
Section: Descriptionmentioning
confidence: 99%
“…12), was sampled for analysis of stable oxygen and carbon isotope geochemistry, using methodology described in Appendix III (online supplement). The results are shown in Of the considerable literature on the stable-oxygen and carbon-isotope chemistry of tufas (Andrews et al, 1993;Andrews, 2006), relatively little is directly related to oncoids (Hagele et al, 2006). Of particular relevance is recent research on modern oncoids in the River Gipping, Ipswich, Suffolk (I.…”
Section: Stable Isotope Geochemistrymentioning
confidence: 90%
“…Conversely, erosion of the channel-bed sediment would have stripped the clasts out of the system and removed them before well-developed overgrowths formed. This is not to say that there was absolutely no sediment movement during the formation of the Purfleet oncoids, as many authors have suggested that clasts need to be turned over regularly to allow formation of the all-enveloping coatings that characterize these carbonates (Hagele et al, 2006).…”
Section: Analysis Of Carbonatesmentioning
confidence: 99%