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- Q3783332 subject Q7034677.
- Q3783332 subject Q7037488.
- Q3783332 subject Q7163796.
- Q3783332 abstract "Carbonate hardgrounds are surfaces of synsedimentarily cemented carbonate layers that have been exposed on the seafloor (Wilson and Palmer, 1992). A hardground is essentially, then, a lithified seafloor. Ancient hardgrounds are found in limestone sequences and distinguished from later-lithified sediments by evidence of exposure to normal marine waters. This evidence can consist of encrusting marine organisms (especially bryozoans, oysters, barnacles, cornulitids, hederelloids, microconchids and crinoids), borings of organisms produced through bioerosion, early marine calcite cements, or extensive surfaces mineralized by iron oxides or calcium phosphates (Palmer, 1982; Bodenbender et al., 1989; Vinn and Wilson, 2010; Vinn and Toom, 2015). Modern hardgrounds are usually detected by sounding in shallow water or through remote sensing techniques like side-scan radar.Carbonate hardgrounds often host a unique fauna and flora adapted to the hard surface. Organisms usually cement themselves to the substrate and live as sessile filter-feeders (Brett and Liddell, 1982). Some bore into the cemented carbonate to make protective domiciles (borings) for filter-feeding. Sometimes hardgrounds are undermined by currents which remove the soft sediment below them, producing shallow cavities and caves which host a cryptic fauna (Palmer and Fürsich, 1974). The evolution of hardground faunas can be traced through the Phanerozoic, from the Cambrian Period to today (Taylor and Wilson, 2003).Carbonate hardgrounds were most commonly formed during calcite sea intervals in Earth history, which were times of rapid precipitation of low-magnesium calcite and the dissolution of skeletal aragonite (Palmer and Wilson, 2004). The Ordovician-Silurian and the Jurassic-Cretaceous Systems have the most hardgrounds (sometimes hundreds in a single section) and the Permian-Triassic Systems have the least (usually none). This cyclicity in hardground formation is reflected in the evolution of hardground-dwelling communities. There are distinct differences between the Paleozoic and Mesozoic hardground communities: the former are dominated by thick calcitic bryozoans and echinoderms, the latter by oysters and deep bivalve (Gastrochaenolites) and sponge (Entobia) borings (Taylor and Wilson, 2003).Stratigraphers and sedimentologists often use hardgrounds as marker horizons and as indicators of sedimentary hiatuses and flooding events (Fürsich et al., 1981, 1992; Pope and Read, 1997). Hardgrounds and their faunas can also represent very specific depositional environments such as tidal channels (Wilson et al., 2005) and shallow marine carbonate ramps (Palmer and Palmer, 1977; Malpas et al., 2004)".
- Q3783332 thumbnail Hardground_oblique_Ordovician_071514c.jpg?width=300.
- Q3783332 wikiPageExternalLink index.html.
- Q3783332 wikiPageExternalLink journal.pone.0134279.
- Q3783332 wikiPageExternalLink index.html.
- Q3783332 wikiPageExternalLink index.html.
- Q3783332 wikiPageExternalLink earth-2015-3-249-253.pdf.
- Q3783332 wikiPageExternalLink PalmerWilson05.pdf.
- Q3783332 wikiPageExternalLink Taylor%26Wilson2003.pdf.
- Q3783332 wikiPageExternalLink ZoharRockyShore.pdf.
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- Q3783332 wikiPageWikiLink Q44626.
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- Q3783332 wikiPageWikiLink Q62412.
- Q3783332 wikiPageWikiLink Q6770636.
- Q3783332 wikiPageWikiLink Q6839384.
- Q3783332 wikiPageWikiLink Q7034677.
- Q3783332 wikiPageWikiLink Q7037488.
- Q3783332 wikiPageWikiLink Q7163796.
- Q3783332 wikiPageWikiLink Q7179161.
- Q3783332 wikiPageWikiLink Q76402.
- Q3783332 wikiPageWikiLink Q79064.
- Q3783332 wikiPageWikiLink Q829.
- Q3783332 comment "Carbonate hardgrounds are surfaces of synsedimentarily cemented carbonate layers that have been exposed on the seafloor (Wilson and Palmer, 1992). A hardground is essentially, then, a lithified seafloor. Ancient hardgrounds are found in limestone sequences and distinguished from later-lithified sediments by evidence of exposure to normal marine waters.".
- Q3783332 label "Carbonate hardgrounds".
- Q3783332 depiction Hardground_oblique_Ordovician_071514c.jpg.