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  • 1
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    Unknown
    In:  galapagosresearch@fcdarwin.org.ec | http://aquaticcommons.org/id/eprint/4183 | 704 | 2011-09-29 16:26:11 | 4183 | Fundacion Charles Darwin Foundation
    Publication Date: 2021-06-30
    Description: David and Lucile Packard Foundation
    Description: Pew Charitable Trust
    Description: Fundación El Viejo
    Keywords: Biology ; Limnology ; freshwater eel ; Anguila marmorata ; Puerto Villamil ; Isla Isabela ; Galápagos
    Repository Name: AquaDocs
    Type: article
    Format: application/pdf
    Format: application/pdf
    Format: 2-6
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  • 2
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    In:  http://aquaticcommons.org/id/eprint/15618 | 8 | 2014-11-10 23:19:39 | 15618
    Publication Date: 2021-07-09
    Description: EXTRACT (SEE PDF FOR FULL ABSTRACT):We have measured coral growth band thickness and skeletal stable isotopic composition through a 371-year transect (AD 1583-1954) from a massive specimen of Pavona clavus from the Galápagos Islands. ... We observe a general cooling trend during 1860-1954, corresponding to the end of the Little Ice Age, an interval characterized by general warming at many mid-latitude sites. Variance at sunspot cycle frequencies in growth rate, stable isotopic, and trace element composition implies a direct or indirect link between the solar cycle and climate modulation in the eastern Pacific.
    Keywords: Atmospheric Sciences ; Chemistry ; Earth Sciences ; Oceanography ; PACLIM
    Repository Name: AquaDocs
    Type: conference_item
    Format: application/pdf
    Format: application/pdf
    Format: 165-178
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  • 3
    Publication Date: 2021-07-10
    Description: EXTRACT (SEE PDF FOR FULL ABSTRACT):Coral-based reconstruction of past variability of sea surface conditions is improving our understanding of the tropical ocean-atmosphere system. We present oxygen isotope records from corals collected near the tip of Baja California (Baja) and the Gulf of Panama (Saboga).
    Keywords: Chemistry ; Oceanography ; PACLIM
    Repository Name: AquaDocs
    Type: conference_item
    Format: application/pdf
    Format: application/pdf
    Format: 203-203
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  • 4
    ISSN: 1432-0975
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Approximately 550 measurements of Mn/Ca ratios in three corals from the western Galapagos Islands have been performed to reconstruct a 380-year history of surface ocean variability with respect to this trace element. The time period studied encompasses 1600 A.D. to 1978. Manganese is inferred to be lattice-bound in coralline aragonite at 10–50% of its seawater proportion to calcium; uncertainty about the distribution coefficient stems from inherent variability of oceanic Mn in nearshore settings. Interannual variations at Urvina Bay, Isabela Island are generally small, with the exception of a few decades during the nineteenth century. A large positive Mn/Ca anomaly found between 1821–1830 is hypothesized to have resulted from a major volcanic eruption on nearby Fernandina Island in 1825. On intrannual timescales a pronounced cycle occurs in response to seasonal upwelling. Quarterly changes in Mn/Ca are six months out-of-phase with Cd/Ca variations-a reflection of the opposite distributions of these metals in the upper waters of the eastern Pacific. High frequency reconstructions over brief time intervals from the 17th, 18th, and 20th century reveal that the seasonal onset of warm and cool phases near Galapagos has persisted for at least 340 years. A quantitative assessment of historical changes in upwelling intensity is complicated by offsets in background Mn levels recorded by different corals. One apparent longterm feature is an overall decline in skeletal Mn concentrations from 1600–1978 which results in a net decrease of 20–30%. Several possible explanations exist for this trend, ranging from accumulation of a persistent diagenetic Mn phase in fossil aragonite to a temporal shift in oceanic/atmospheric Mn fluxes reaching the surface waters of the Galapagos Islands.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 368 (1994), S. 697-697 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] GLEASON AND WELLINGTON REPLY - Dunne suggests that we were premature in attributing the coral bleaching we observed in our experiments1 to ultraviolet radiation because we did not take into account an 8% difference in PAR between treatments with and without ultraviolet; and because we did not ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 365 (1993), S. 836-838 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A large proportion of the Caribbean corals that bleached during 1987 and 1990 were found at depths greater than 20 m. To determine whether increased ultraviolet (UV) radiation in the 280-400-nm band could have contributed to these bleaching uble protein per cm2 of coral tissue surface (Fig. 2c and ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 293 (1981), S. 453-455 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Thus far, most studies of isotopic and chemical variation in hermatypic corals, and all studies of seasonal isotopic variation, have involved species with massive growth habits, partly because such corals often produce annual24 dense bands which can be used as time markers. For examination of ...
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Coral reefs 1 (1983), S. 215-222 
    ISSN: 1432-0975
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract The timing of skeletal band formation and concomitant changes in calcification rates and linear skeletal extension were investigated in Pavona corals growing under two distinct thermal regimes along the Pacific coast of Panama: fluctuating, marked by seasonal upwelling (Gulf of Panama) and stable, nonupwelling (Gulf of Chiriqui). The purpose of this study was to test the hypothesis that banding in corals is largely mediated by seasonal variations in temperature (Highsmith 1979). Our results indicate that the timing of band formation is synchronous at these two environmentally distinct locations. The low density (LD) portion of the annual band is accreted over a five month period (January–June) and represents an increase in linear skeletal extension (mm/mo.) as well as a marked increase in calcification rate (g CaCO3 · cm-2 · mo-1) relative to the high density portion which forms over the remaining seven month period (July through December). In contrast to the predictions of the Highsmith model these findings indicate that variations in light levels rather than fluctuation in temperature is a better correlate to changes in skeletal density. Qualitatively, banding patterns were similar at the two sites; however, higher growth rates (particularly with respect to the LD band) for Pavona clavus in the Gulf of Panama indicate that lower water temperatures and higher productivity, or both, may be responsible for quantitative differences in banding between sites. We found that formation of the HD band corresponds to lower light levels and the production of gametes. We propose that banding in corals is a complex phenomenon governed by endogenous processes (e.g. reallocation of energy from growth to reproduction) which may be mediated by exogenous factors (e.g light and productivity).
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Oecologia 52 (1982), S. 311-320 
    ISSN: 1432-1939
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary In Panamá, vertical zonation of coral species is well marked; branching corals (Pocillopora spp.) predominate in shallow (1–6 m) water while massive forms (Pavona spp.) occupy the deeper (6–10 m) areas of the reef. To test the hypothesis that this zonation represents differential resource utilization (i.e., niche partitioning of food resources), one year manipulative field experiments were conducted at two depths (1 m and 7 m below Mean Lower Sea Level) assessing the relative contribution of light and zooplankton to the nutrition of three Pacific corals: Pocillopora damicornis, Pavona clavus and Pavona gigantea. Also tested were the related hypotheses that (i) energy for the maintenance and growth of corals comes mainly from light, independent of zooplankton supply and (ii) Porter's model, in which coral morphology is a predictor of the phototrophic-heterotrophic capabilities of a particular species. That is, corals with a branching morphology and a small polyp diameter (and short tentacle length) should be primarily phototrophic while those species with larger polyps and/or a massive form should show a greater degree of heterotrophy. The comparison of caged versus control corals indicated that the branching coral, Pocillopora damicornis (polyp diameter — 1 mm) grew independent of zooplankton supply (〉95μ) but was markedly affected by shading. Pavona clavus (massive form with intermediate size polyps — 2 mm) was also negatively affected by shading but this effect was minimized when zooplankton was present. Surprisingly, under ambient light conditions, the growth of this specics was independent of zooplankton (〉95μ); perhaps indicating a facultative reliance on zooplankton especially in shallow water. The third species, Pavona gigan-tea (massive form with largest polyps — 3 mm) was highly dependent on both light and zooplankton and was unable to compensate for the effects of shading by zooplankton feeding. This high dependence on light was unexpected since large polyps, according to Porter's model, would predict a more heterotrophic existence. Under all treatments, in both shallow and deep water, Pocillopora was found to grow more rapidly than either massive species. Thus, this study indicates that zonation on eastern Pacific reefs cannot be explained by depth-related differences in nutritional requirements among the species present. These results do provide the first long-term, experimental field evidence that corals are largely phototrophic organisms. The validity of Porter's model attempting to correlate phototrophic-heterotrophic abilities to morphological characteristics is, at least, partially verified: species with larger tentacles do appear to utilize zooplankton to a greater extent than those species with smaller tentacles. However, the significance of corallum morphology in predicting the mode of nutrient acquisition is unclear. Rather, behavioral patterns (tentacle expansion-contraction cycles) and location on the reef may be more important factors to consider.
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  • 10
    ISSN: 1432-1939
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The mass mortality of reef corals in the eastern Pacific as a result of the 1982–1983 El Niño oceanographic anomaly permitted the first large scale test of resource limitation for a coral reef fish. Population densities of territorial herbivorous damselfish did not respond to the massive regional increase in space available for the cultivation of algal food following the El Niño event. The proportion of juveniles in the population was low and new recruits were uncommon, indicating that recruitment rates rather than resource supply probably control the abundance of this coral reef damselfish.
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