Article citations

    Mayfield, A.B., Hsiao, Y.Y., Fan, T.Y., Chen, C.S. and Gates, R.D. (2010) Evaluating the Temporal Stability of Stress-Activated Protein Kinase and Cytoskeleton Gene Expression in the Pacific Corals Pocillopora damicornis and Seriatopora hystrix. Journal of Experimental Marine Biology and Ecology, 395, 215-222.

has been cited by the following article:

  • TITLE: Exploring the Environmental Physiology of the Indo-Pacific Reef Coral <em>Seriatopora hystrix</em> with Differential Proteomics
  • AUTHORS: Anderson B. Mayfield, Yi-Jyun Chen, Chi-Yu Lu, Chii-Shiarng Chen
  • KEYWORDS: Acclimation, Coral Reefs, Dinoflagellate, Environmental Physiology, Marine Biology, Marine Invertebrates, Molecular Biology, Proteomics, Taiwan
  • JOURNAL NAME: Open Journal of Marine Science DOI: 10.4236/ojms.2018.82012 May 15, 2018
  • ABSTRACT: Although reef-building corals are threatened by a number of anthropogenic impacts, certain scleractinian-dinoflagellate (genus Symbiodinium) endosymbioses have proven markedly resilient to environmental change. For instance, corals from upwelling habitats of Southern Taiwan withstand both short- and long-term increases in temperature, potentially due to their routine exposure to highly variable temperature regimes in situ. To gain a greater understanding of the proteomic basis for such acclimatization to unstable environmental conditions, specimens of the Indo-Pacific reef-building coral Seriatopora hystrix Dana 1846 were sampled during a period of stable temperature conditions from 1) a site characterized by frequent upwelling events in Southern Taiwan and 2) a nearby, non-upwelling control site in the Taiwan Strait. Two-dimensional gel electrophoresis followed by sequencing of differentially concentrated proteins with mass spectrometry unveiled significantly more proteins involved in the cellular stress response in coral hosts of the upwelling site. Although such stress protein signatures could be indicative of sub-lethal levels of cellular stress, especially given the relatively higher sediment loads characteristic of the upwelling site, these proteins may, in contrast, have been constitutively maintained at high levels in preparation for large fluctuations in temperature and other abiotic parameters (e.g., nutrient levels) brought upon by upwelling events.