Gibson V L, Richards Donà A, Smith C M
School of Life Sciences, University of Hawai'i at Mānoa, 310 Maile Way, St John 101, Honolulu, HI 96822, USA.
Water Resources Research Center, University of Hawai'i at Mānoa, 2540 Dole Street, Holmes Hall 293, Honolulu, HI 96822, USA.
AoB Plants. 2023 Aug 22;15(5):plad055. doi: 10.1093/aobpla/plad055. eCollection 2023 Oct.
Regulation of tissue water potential is a key mechanism in macroalgal osmotic responses to changing external osmotic conditions, which are common in tidally influenced estuarine and intertidal systems. Nevertheless, significant knowledge gaps exist in our understanding of osmotic responses in macroalgae because few methods measure osmotic potential within macroalgal tissues. Leaf psychrometers have furthered understanding of osmotic potentials in terrestrial plant water relations, yet these have not been developed to measure the range of highly negative potential values found in marine macroalgae. To address these gaps, we present an effective, updated version of the Chardakov method to measure tissue water potential in macroalgae. Here, we present a case study examining macroalgal response in tissue water potential by two morphologically and evolutionarily distinct species, (Chlorophyta) and (Rhodophyta) to four paired salinity and nutrient treatments at two temperatures. These treatments simulate a gradient from full coastal ocean conditions to brackish submarine groundwater discharge, an ecosystem type found on basaltic shorelines. Both algae demonstrated plasticity in osmotic response to submarine groundwater discharge with significant positive correlations between tissue water potential and proportion of submarine groundwater discharge in the treatment. These results are the first to describe macroalgal response in tissue water potential, a first step to understanding algal physiological ecology in such complex coastal environments. This revised Chardakov method is a valuable tool to better understand species-specific osmotic responses to ecologically relevant conditions, and can augment the study of other tidal systems and ontogenetic stages.
组织水势的调节是大型海藻对外部渗透条件变化的渗透反应中的关键机制,这种变化在受潮汐影响的河口和潮间带系统中很常见。然而,我们对大型海藻渗透反应的理解存在重大知识空白,因为很少有方法能测量大型海藻组织内的渗透势。叶片湿度计增进了我们对陆地植物水分关系中渗透势的理解,但尚未开发出能测量海洋大型海藻中发现的高度负势值范围的仪器。为填补这些空白,我们提出了一种有效且更新的查尔达科夫方法来测量大型海藻的组织水势。在此,我们展示一个案例研究,考察两种形态和进化上不同的物种,绿藻门的 和红藻门的 ,在两种温度下对四组配对的盐度和营养处理的组织水势中的大型海藻反应。这些处理模拟了从完全的沿海海洋条件到微咸的海底地下水排放的梯度,这是玄武岩海岸线上发现的一种生态系统类型。两种藻类在对海底地下水排放的渗透反应中都表现出可塑性,在处理中组织水势与海底地下水排放比例之间存在显著正相关。这些结果首次描述了大型海藻在组织水势方面的反应,是理解此类复杂沿海环境中藻类生理生态学的第一步。这种修订后的查尔达科夫方法是一个有价值的工具,可更好地理解物种对生态相关条件的特定渗透反应,并可加强对其他潮汐系统和个体发育阶段的研究。