26
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: not found

      Pelagic Sargassum community change over a 40-year period: temporal and spatial variability

      research-article
      , , , ,
      Marine Biology
      Springer Berlin Heidelberg

      Read this article at

      ScienceOpenPublisherPMC
      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Pelagic forms of the brown algae (Phaeophyceae) Sargassum spp. and their conspicuous rafts are defining characteristics of the Sargasso Sea in the western North Atlantic. Given rising temperatures and acidity in the surface ocean, we hypothesized that macrofauna associated with Sargassum in the Sargasso Sea have changed with respect to species composition, diversity, evenness, and sessile epibiota coverage since studies were conducted 40 years ago. Sargassum communities were sampled along a transect through the Sargasso Sea in 2011 and 2012 and compared to samples collected in the Sargasso Sea, Gulf Stream, and south of the subtropical convergence zone from 1966 to 1975. Mobile macrofauna communities exhibited changes in community structure and declines in diversity and evenness within a 6-month time period (August 2011–February 2012). Equivalent declines in diversity and evenness were recorded in the same region (Sargasso Sea, 25°–29°N) in 1972–1973. Recent community structures were unlike any documented historically, whether compared to sites of the same latitude range within the Sargasso Sea, or the broader historical dataset of sites ranging across the Sargasso Sea, Gulf Stream, and south of the subtropical convergence zone. Recent samples also recorded low coverage by sessile epibionts, both calcifying forms and hydroids. The diversity and species composition of macrofauna communities associated with Sargassum might be inherently unstable. While several biological and oceanographic factors might have contributed to these observations, including a decline in pH, increase in summer temperatures, and changes in the abundance and distribution of Sargassum seaweed in the area, it is not currently possible to attribute direct causal links.

          Electronic supplementary material

          The online version of this article (doi:10.1007/s00227-014-2539-y) contains supplementary material, which is available to authorized users.

          Related collections

          Most cited references69

          • Record: found
          • Abstract: not found
          • Article: not found

          Projecting global marine biodiversity impacts under climate change scenarios

            Bookmark
            • Record: found
            • Abstract: found
            • Article: not found

            Global trends in wind speed and wave height.

            Studies of climate change typically consider measurements or predictions of temperature over extended periods of time. Climate, however, is much more than temperature. Over the oceans, changes in wind speed and the surface gravity waves generated by such winds play an important role. We used a 23-year database of calibrated and validated satellite altimeter measurements to investigate global changes in oceanic wind speed and wave height over this period. We find a general global trend of increasing values of wind speed and, to a lesser degree, wave height, over this period. The rate of increase is greater for extreme events as compared to the mean condition.
              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              Green and golden seaweed tides on the rise.

              Sudden beaching of huge seaweed masses smother the coastline and form rotting piles on the shore. The number of reports of these events in previously unaffected areas has increased worldwide in recent years. These 'seaweed tides' can harm tourism-based economies, smother aquaculture operations or disrupt traditional artisanal fisheries. Coastal eutrophication is the obvious, ultimate explanation for the increase in seaweed biomass, but the proximate processes that are responsible for individual beaching events are complex and require dedicated study to develop effective mitigation strategies. Harvesting the macroalgae, a valuable raw material, before they beach could well be developed into an effective solution.
                Bookmark

                Author and article information

                Contributors
                +1-831-775-1839 , chuffard@mbari.org
                Journal
                Mar Biol
                Mar. Biol
                Marine Biology
                Springer Berlin Heidelberg (Berlin/Heidelberg )
                0025-3162
                1432-1793
                14 September 2014
                14 September 2014
                2014
                : 161
                : 12
                : 2735-2751
                Affiliations
                [ ]Monterey Bay Aquarium Research Institute, 7700 Sandholdt Rd, Moss Landing, CA 95039 USA
                [ ]Coastal Ecology Laboratory, Biology Department, University of Miami, Coral Gables, FL 33124 USA
                Author notes

                Communicated by F. Bulleri.

                Article
                2539
                10.1007/s00227-014-2539-y
                4231207
                25414525
                56b0b92f-041f-401c-985e-21e8a7bfa5c8
                © The Author(s) 2014

                Open AccessThis article is distributed under the terms of the Creative Commons Attribution License which permits any use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited.

                History
                : 20 May 2014
                : 3 September 2014
                Categories
                Original Paper
                Custom metadata
                © Springer-Verlag Berlin Heidelberg 2014

                Comments

                Comment on this article