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  • 1
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Ecology, Evolution, and Systematics 17 (1986), S. 273-303 
    ISSN: 0066-4162
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Coral reefs 16 (1997), S. 29-37 
    ISSN: 1432-0975
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract.  An algal ridge system discovered along the Exuma Cays, Bahamas constructs bioherms to a thickness of at least 1.5 m and is associated with modern intertidal stromatolites. These algal ridges are unique because they grow in atypical environments characterized by relatively low wave energy, high rates of sedimentation and low rates of herbivory. They also are composed primarily of the branching crustose coralline alga, Neogoniolithon strictum, which heretofore was not known to form algal ridges. Lateral growth rates of crusts, vertical growth rates of branches and survivorship of transplanted N. strictum were greatest in the shallow fore reef zone of the algal ridge. The alga is also capable of surviving and growing when covered with sediment for at least 100 days. Under such conditions it transforms from a branched to an unbranched morphology. Parrotfish grazing, which is said to limit the abundance of branched corallines and algal ridges, was two orders of magnitude lower than in published accounts from other reef systems of the Caribbean and one order of magnitude less than that found on nearby coral reefs of the west Exuma Sound. Neogoniolithon strictum, a delicate and open-branched coralline, persisted for over a year without grazing damage when transplanted to a depth of 2.3 m. This algal ridge-building coralline becomes a well-indurated limestone following submarine lithification of sediment that infills the open branch framework. As a result, N. strictum ridges are comparable to the dense frameworks associated with most algal ridges. Observations of N. strictum -associated bioherms along Central America suggest this ridge system may exist elsewhere under conditions similar to those described for the Bahamas.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-0975
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences
    Notes: Abstract Submersible observations and collections reveal that a probable relict reef off the west coast of Barbados has a rich cover of sponges, along with algae and scattered corals, on a substrate of algal nodules in a muddy-sand matrix. The collections provide new data on the distributions of these fauna. This relict reef is about 20 km long, has a relief of up to 10 m, and is established at a depth of 80 m. Relict shallow-water features in other areas at similar depths along with data from core holes drilled off the south coast of Barbados suggest that this reef was probably established about 12,000 years ago and existed for no more than 2,000 years, during the Holocene sea-level transgression.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 68 (1982), S. 299-319 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The susceptibility of an alga to an herbivorous mollusc depends, in part, upon the size and toughness of the plant relative to the feeding ability of the mollusc. In this study, algae are subdivided into seven functional groups based on these and other physiological characteristics. Herbivorous prosobranchs and chitons are subdivided into four functional groups based on the structure of their feeding apparatus. Distinct patterns in the diets of these molluscs are evident when feeding data, based on these functional groups, are examined. Most herbivorous mollusc species eat algal forms that are either minute (i.e., micro- and filamentous algae) or very large and expansive (kelp-like or crustose algae). Algae of intermediate size (erect forms 1- to 10-cm tall) are eaten to a lesser extent, possibly because they are too large to be rasped from the substratum and too small for most herbivores to occupy. Herbivorous archaeogastropods (excluding limpets) and mesogastropods tend to eat filamentous and microscopic algal forms predominantly, whereas limpets and chitons feed on large, leathery and crustose algae. These dietary differences reflect functional differences in the feeding apparatus of these herbivore groups. Radulae of herbivorous mesogastropods function like rakes and can ingest larger, tougher algae than can radulae of nonlimpet archaeogastropods. The latter function more like brooms by sweeping the substratum broadly, but exerting little force. Limpets and chitons have superior excavating abilities because their radulae have: robust buccal muscles surrounding them, a reduced number of points of contact on the substratum, and minerally hardened teeth. The feeding apparatus of chitons is most versatile since it possesses features found in all herbivorous gastropod functional groups, and thus, it can sweep and excavate simultaneously. This functional group approach suggests various hypotheses concerning algal community structure, plant/herbivore and herbivore/herbivore interactions, the relative importance of structural defenses in algae, and the evolution of specialized grazers. These hypotheses are examined using data from published accounts.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2021-02-08
    Description: The potential of crustose coralline algae as high-resolution archives of past ocean variability in mid- to high-latitudes has only recently been recognized. Few comparisons of coralline algal proxies, such as temperature-dependent algal magnesium to calcium (Mg/Ca) ratios, with in situ-measured surface ocean data exist, even rarer are well replicated records from individual sites. We present Mg/Ca records from nine coralline algal specimens (Clathromorphum compactum) from a single site in the Gulf of Maine, North Atlantic. Sections from algal mounds were analyzed using Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) yielding individual Mg/Ca records of up to 30 years in length. We first test intra- and intersample signal replication and show that algal Mg/Ca ratios are reproducible along several transects within individual sample specimens and between different samples from the same study site. In addition, LA-ICP-MS-derived Mg/Ca ratios are compared to electron microprobe (EMP) analyzed data on the longest-lived specimens and were found to be statistically commensurable. Second, we evaluate whether relationships between algal-based SST reconstructions and in situ temperature data can be improved by averaging Mg/Ca records from multiple algal specimens (intersample averages). We found that intersample averages yield stronger relationships to sea surface temperature (SST) data than Mg/Ca records derived from individual samples alone. Thus, Mg/Ca-based paleotemperature reconstructions from coralline algae can benefit from using multiple samples per site, and can expand temperature proxy precision from seasonal to monthly.
    Type: Article , PeerReviewed
    Format: text
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  • 6
    Publication Date: 2017-06-19
    Description: Higher latitude oceanic and climatic reconstructions are needed to distinguish natural climate variability from anthropogenic warming in regions projected to experience significant increases in temperature during this century. Clathromorphum nereostra turn is a long-lived coralline alga abundant along the Aleutian archipelago that records seasonal to centennial fluctuations in seawater temperatures in its high-Mg calcite skeleton. Thus, C. nereostratum is an important proxy archive to reconstruct past seawater temperature variability in this data-poor subarctic region. Here, we measured magnesium to calcium ratios (Mg/Ca) by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) along the growth axis in six live-collected specimens from three islands in the Aleutian archipelago to assess Mg/Ca reproducibility and to calibrate algal Mg/Ca against modern gridded sea surface temperature (SST) data products. The master Mg/Ca SST transfer function, determined by averaging the algal Mg/Ca SST from each island (n = 6), resulted in a reconstruction error of +/-0.45 degrees C, a 31-46% reduction in error compared to the reconstruction error for a single alga. The master algal-SST record interpolated to monthly and annual resolution significantly varied with gridded SST data products (r(2) = 0.98, p 〈 0.0001, n = 517 and r(2) = .27, p 〈 0.0003, n = 44, respectively) for the period from 1960 to 2003. Therefore, coralline algal Mg/Ca-derived SST reconstructions record absolute changes in past SST variability in the Aleutian archipelago. The transfer functions developed here can be applied to Mg/Ca records generated from long-lived specimens of C. nereostra turn to reconstruct northern North Pacific and Bering Sea SST variability for the past several hundred years.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Format: text
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  • 7
    Publication Date: 2017-12-07
    Type: Article , PeerReviewed
    Format: text
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  • 8
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    In:  [Poster] In: EGU General Assembly 2009, 19.-24.04.2009, Vienna, Austria . Geophysical Research Abstracts ; EGU2009-3852-2 .
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
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    In:  [Poster] In: AGU Fall Meeting 2012, 03.-07.12.2012, San Francisco, USA .
    Publication Date: 2012-12-12
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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