Marine Spatial Ecology Lab, School of Biological Sciences and ARC Centre of Excellence for Coral Reef Studies, University of Queensland, St Lucia, Qld, Australia.
School of Medical Sciences, University of Sydney, Sydney, NSW, Australia.
Glob Chang Biol. 2020 Jul;26(7):3858-3879. doi: 10.1111/gcb.15103. Epub 2020 Apr 30.
Coastal and intertidal habitats are at the forefront of anthropogenic influence and environmental change. The species occupying these habitats are adapted to a world of extremes, which may render them robust to the changing climate or more vulnerable if they are at their physiological limits. We characterized the diurnal, seasonal and interannual patterns of flux in biogeochemistry across an intertidal gradient on a temperate sandstone platform in eastern Australia over 6 years (2009-2015) and present a synthesis of our current understanding of this habitat in context with global change. We used rock pools as natural mesocosms to determine biogeochemistry dynamics and patterns of eco-stress experienced by resident biota. In situ measurements and discrete water samples were collected night and day during neap low tide events to capture diurnal biogeochemistry cycles. Calculation of pH using total alkalinity (TA) and dissolved inorganic carbon (DIC) revealed that the mid-intertidal habitat exhibited the greatest flux over the years (pH 7.52-8.87), and over a single tidal cycle (1.11 pH units), while the low-intertidal (pH 7.82-8.30) and subtidal (pH 7.87-8.30) were less variable. Temperature flux was also greatest in the mid-intertidal (8.0-34.5°C) and over a single tidal event (14°C range), as typical of temperate rocky shores. Mean TA and DIC increased at night and decreased during the day, with the most extreme conditions measured in the mid-intertidal owing to prolonged emersion periods. Temporal sampling revealed that net ecosystem calcification and production were highest during the day and lowest at night, particularly in the mid-intertidal. Characterization of biogeochemical fluctuations in a world of extremes demonstrates the variable conditions that intertidal biota routinely experience and highlight potential microhabitat-specific vulnerabilities and climate change refugia.
沿海和潮间带生境处于人为影响和环境变化的前沿。这些生境中的物种适应了极端的世界,这可能使它们对气候变化具有更强的适应能力,或者如果它们处于生理极限,它们就更容易受到影响。我们在 6 年(2009-2015 年)的时间里,在澳大利亚东部一个温带砂岩平台的潮间带梯度上,对生物地球化学通量的日、季和年际模式进行了描述,并结合全球变化对这一栖息地的现有认识进行了综合分析。我们使用岩石池作为自然中间容器来确定生物地球化学动力学和驻留生物经历的生态压力模式。在低潮期间,白天和黑夜都进行了原位测量和离散水样采集,以捕捉日生物地球化学循环。使用总碱度(TA)和溶解无机碳(DIC)计算 pH 值表明,多年来中潮带生境表现出最大的通量(pH 值为 7.52-8.87),并且在单个潮汐周期内(1.11 pH 单位),而低潮带(pH 值为 7.82-8.30)和亚潮带(pH 值为 7.87-8.30)的变化较小。中潮带的温度通量也最大(8.0-34.5°C),在单个潮汐事件中(14°C 范围)也是如此,这是温带多岩石海岸的典型特征。TA 和 DIC 的平均值在夜间增加,白天减少,中潮带的条件最为极端,因为长时间的暴露期。时间采样表明,净生态系统钙化和生产力在白天最高,在夜间最低,尤其是在中潮带。在极端世界中生物地球化学波动的特征表明,潮间带生物经常经历的条件是多变的,并突出了潜在的微生境特异性脆弱性和气候变化避难所。