دورية أكاديمية

Global warming offsets the ecophysiological stress of ocean acidification on temperate crustose coralline algae.

التفاصيل البيبلوغرافية
العنوان: Global warming offsets the ecophysiological stress of ocean acidification on temperate crustose coralline algae.
المؤلفون: Kim, Ju-Hyoung, Kim, Nahyun, Moon, Hanbi, Lee, Sukyeon, Jeong, So Young, Diaz-Pulido, Guillermo, Edwards, Matthew S., Kang, Ju-Hyun, Kang, Eun Ju, Oh, Hyun-Ju, Hwang, Jae-Dong, Kim, Il-Nam
المصدر: Marine Pollution Bulletin; Aug2020, Vol. 157, pN.PAG-N.PAG, 1p
مصطلحات موضوعية: OCEAN acidification, CORALLINE algae, GLOBAL warming, HIGH temperatures, CLIMATE change, TEMPERATE climate
مستخلص: Dramatic increases in the release of anthropogenic CO 2 and global temperatures have resulted in alterations to seawater carbonate chemistry and metabolisms of marine organisms. There has been recent interest in the effects of these stressors on crustose coralline algae (CCA) because photosynthesis and calcification are influenced by all components of carbonate chemistry. To examine this, a mesocosm experiment was conducted to evaluate photosynthesis, calcification and growth in the temperate CCA Chamberlainium sp. under acidification (doubled CO 2), warming (+5 °C), and greenhouse (doubled CO 2 and +5 °C) conditions compared to present-day conditions. After 47 days of acclimation to these conditions, productivity was lowest under acidification, although photochemical properties were improved, while respiration was highest under warming. Likewise, growth was lowest under acidification, but this negative response was offset by elevated temperature under greenhouse. Together, these results suggest that warming offsets the negative effects of acidification by creating more suitable conditions for photosynthesis and growth. • The ecological risk of climate change on temperate CCA has been assessed by mesocosm. • Future change in carbonate chemistry has led to ecophysiological change of CCA. • Oxygenic photosynthesis and growth decreased under acidified seawater. • Negative metabolic changes in ocean acidification were offset by elevated temperature. [ABSTRACT FROM AUTHOR]
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قاعدة البيانات: Supplemental Index
الوصف
تدمد:0025326X
DOI:10.1016/j.marpolbul.2020.111324