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  • 1
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    In:  EPIC32015 Aquatic Sciences Meeting - Aquatic Sciences: Global And Regional Perspectives — North Meets South, Granada, Spain, 2015-02-22-2015-02-27
    Publication Date: 2016-03-01
    Description: Most of what is known about the effects of ocean acidification on zooplankton relates to a few species composed of calcium carbonate, or comes from laboratory and mesocosm studies that observe a relatively small number of species, primarily copepods. So far little is known about how entire zooplankton communities may change due to elevated carbon dioxide levels. We examined changes in zooplankton residential to coral reefs at two reefs in Papua New Guinea where underwater seeps create a natural pH gradient. Traditional net tows, emergence traps, and acoustical instruments were used to collect and observe zooplankton over three separate seasons and emerging from different types of substrata. All methods indicated a dramatic loss in zooplankton abundance where pH was reduced to 7.8 compared to healthy reefs with a normal pH of 8.1. We observed both changes in the overall zooplankton community, and examined each taxonomic group separately to investigate differences in the sensitivity between taxonomic groups. Reduced quantities of zooplankton will likely affect marine organisms that feed on them.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 2
    Publication Date: 2017-06-08
    Description: Crustose coralline algae (CCA) fulfill important ecosystem functions in coral reefs, including reef framework stabilization and induction of larval settlement. To investigate in situ the effects of high carbon dioxide on CCA communities, we deployed settlement tiles at three tropical volcanic CO2 seeps in Papua New Guinea along gradients spanning from 8.1 to 7.4 pH. After 5 and 13 months deployment, there was a steep transition from CCA presence to absence around pH 7.8 (660 μatm pCO2): 98% of tiles had CCA at pH 〉 7.8, whereas only 20% of tiles had CCA at pH ≤ 7.8. As pH declined from 8.0 to 7.8, the least and most sensitive CCA species lost 43% and 85% of cover, respectively. Communities on upward facing surfaces exposed to high light and high grazing pressure showed less steep losses than those on shaded surfaces with low grazing. Direct CO2 effects on early life stages were the main mechanisms determining CCA cover, rather than competitive interactions with other benthic groups. Importantly, declines were steepest at near-ambient pH, suggesting that CCA may have already declined in abundance due to the recent seawater pH decline of 0.1 units, and that future severe losses are likely with increasing ocean acidification.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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