Collaborative Research: The effect of carbonate chemistry on the sea ice community in the High Arctic

海冰影响北极发生的许多物理、大气、化学和生物过程。海冰也是一个具有挑战性的栖息地评估：它移动响应风，因此几乎总是独立于表面沃茨移动。冰的性质会影响大气、冰和海洋表面之间的一系列化学和生物相互作用，这些性质会随着空间和时间的变化而变化。虽然在越来越无冰的北冰洋中预计会增强光合作用，但很少有研究来确定大气二氧化碳（CO2）增加和其他环境变化对海冰内和海冰下生长的微生物的影响。这项研究将有助于我们了解北极盆地中部的元素循环，以及海冰生物群落对迅速变化的环境的脆弱性，特别是因为它受到二氧化碳浓度增加和海洋酸化的影响。该项目是美国和瑞典联合合作的一部分，将支持一名早期职业女性教师。它还将支持培训一名研究生和一名博士后科学家，他们将获得进行中和离散地球化学取样以及孵化实验的经验。调查人员将在西雅图太平洋科学中心举行的VIMS海洋科学日和极地科学周末活动上对北冰洋的变化进行公众宣传。这项研究的总体目标是评估大气二氧化碳（CO2）增加导致的海水化学变化如何改变海冰中的藻类-细菌相互作用。最近北极海冰的减少导致大气中二氧化碳的吸收增加，加速了这个正在迅速变化的地区的酸化速度。虽然预计北极日益无冰将提高海洋生产力，但不断变化的环境对依赖冰的生物群落的影响难以预测。作为美国和瑞典联合合作的一部分，这项工作将对依赖冰的藻类和细菌对pH值变化的敏感性进行定量评估，并结合进行中和离散采样，对高北极地区夏末海冰最少时二氧化碳系统的时空变化进行新的观察。此外，研究小组还将进行一系列船上实验，控制海水pH值，以评估对海冰生物群及其外聚合物多糖产品的影响。虽然以前的工作主要集中在二氧化碳浓度升高对浮游植物的影响，但很少有针对性的研究依赖冰的生物群。鉴于北极海盆中部CO2系统观测的缺乏，特别是在生产季节的后期，秋季生产的影响和季节性盐度最低值可以包括在生产的累积估计中，这里提出的观测将具有特别的意义。

Sea ice influences many physical, atmospheric, chemical and biological processes occurring in the Arctic. Sea ice is also a challenging habitat to assess: it moves in response to wind, and hence nearly always moves independently of surface waters. The properties of the ice, which influence a suite of chemical and biological interactions between the atmosphere, the ice, and the surface ocean, change over both space and time. While enhanced photosynthesis is expected in the increasingly ice-free Arctic Ocean, there has been little research to determine the impact of increased atmospheric carbon dioxide (CO2) and other environmental changes on the microbes that grow within and beneath the sea ice. This research will contribute to our understanding of elemental cycles in the central Arctic basin and of the vulnerability of the sea ice biological community to a rapidly changing environment, particularly as it is impacted by increasing carbon dioxide concentrations and ocean acidification. The project is part of a joint US-Swedish collaboration and will support an early-career female faculty member. It will also support the training of a graduate student and a postdoctoral scientist who will gain experience with underway and discrete biogeochemical sampling as well as incubation experiments. The investigators will conduct public outreach about changes in the Arctic Ocean at the VIMS Marine Science Day and Polar Science Weekend at the Pacific Science Center in Seattle. The overall objective of this research is to assess how changes in seawater chemistry as a result of increases in atmospheric carbon dioxide (CO2) will alter algal-bacterial interactions in sea ice. Recent losses of Arctic sea ice have resulted in an increased uptake of atmospheric CO2, accelerating the rate of acidification in a region that is rapidly changing. While enhanced marine productivity is expected in an increasingly ice-free Arctic, the impact of the changing environment on ice-dependent biological communities is challenging to predict. As part of a joint US-Swedish collaboration, this work will provide a quantitative assessment of the sensitivity of ice-dependent algae and bacteria to changes in pH and use a combination of underway and discrete sampling to deliver new observations on the spatial and temporal variability of the CO2 system in the High Arctic in late summer when sea ice is at a minimum. In addition, the research team will perform a suite of ship-board experiments that manipulate seawater pH to assess the impacts on sea ice biota and their exopolymer polysaccharide products. Although previous work has focused on the impact of elevated CO2 on phytoplankton, there has been little targeted research on ice-dependent biota. Given the paucity of CO2 system observations in the central Arctic basin, especially late in the productive season when the impact of autumn production and the seasonal salinity minimum can be included in the cumulative estimate of production, the observations proposed here will be of particular significance.