1999
DOI: 10.1016/s0967-0637(98)00083-1
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Hydrography and geostrophy around Easter Island

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Cited by 14 publications
(8 citation statements)
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“…Silica has usually been observed to be higher than nitrate, shows little fluctuation in surface gyre waters, and has been suggested not to be a limiting nutrient (discussed above), so silica would not be expected to explain these changes. Also, the lowest silica concentrations reported (<0.8 µmol L -1 ) are near Easter Island (Moraga et al, 1999), possibly indicating consumption by diatoms. Dinoflagellates showed no similar patterns in composition (Fig.…”
Section: Analysis Of a Possible Island-mass Effect Around Easter Islamentioning
confidence: 93%
“…Silica has usually been observed to be higher than nitrate, shows little fluctuation in surface gyre waters, and has been suggested not to be a limiting nutrient (discussed above), so silica would not be expected to explain these changes. Also, the lowest silica concentrations reported (<0.8 µmol L -1 ) are near Easter Island (Moraga et al, 1999), possibly indicating consumption by diatoms. Dinoflagellates showed no similar patterns in composition (Fig.…”
Section: Analysis Of a Possible Island-mass Effect Around Easter Islamentioning
confidence: 93%
“…The island hosts a diverse algal population (Santelices and Abbott, 1988), but its primary production is limited by low nutrient levels in the water typical of the mid-Southeast Pacific gyre in which it is situated (Moraga et al, 1999). The island's leafy algal species, primarily Sargassum skottsbergi and Zonaria stipitata, are unpalatable for most fishes and invertebrates as indirectly suggested by our personal observations, data reported below, and Duhart and Ojeda (1994).…”
Section: Introductionmentioning
confidence: 76%
“…Since our survey publication (DiSalvo et al, 1988), new data have become available on oceanographic characteristics of the sea around Easter Island, including nutrients, temperature and currents (Moraga et al, 1999). Other studies have added knowledge of faunal groups of the island such as the sponges (Desqueyroux-Faundez, 1990), corals (Glynn et al, 2003), molluscs (Raines, 2002) and macrocrustaceans (Poupin, 2003) as well as certain less conspicuous groups including the Foraminifera (Zapata and Olivares 2000), the Ostracoda (Whatley et al, 2000) and the Isopoda (Kensley, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…Winds blow throughout the year and are predominantly from east−southeast, but the influence of strong easterlies on the ocean surface can be felt even on the leeward northwest coast as energy is refracted and diffracted around the tips of the island. Unfortunately, local nearshore circulation patterns around the island are unknown, although surface circulation in the region is generally east to west (Glynn et al 2007), and the island itself does modify the predominantly northwestern large-scale geostrophic flows (Moraga et al 1999). Like most sites along the western and northern coasts where coral communities are particularly well developed, Tautara is characterized by overall high coral cover (80%), with Pocillopora verrucosa and Porites lobata contributing similarly to total coral abundance (see Wieters et al 2014 for quantitative description of temporal and geographic patterns in functional structure and coral abundances around the island).…”
Section: Study Sitementioning
confidence: 99%