Yan Zhao

Ocean acidification (OA) significantly alters the carbonate chemistry of seawater, leading to a decrease of seawater pH to impact the physiological and biochemical processes of those intertidal macroalgae. Previous studies have focused on the response of macroalgae to OA at thallus stage, while the effects at filamentous stage remain insufficiently explored. This study investigated the physiological-biochemical and molecular mechanisms of the filamentous conchocelis stage (the diploid sporophyte) of Neopyropia yezoensis responding to short- (5 days) and long-term (20 days) OA (2000 ppm CO2, pH 7.53). The results showed that short-term OA rapidly inhibited the growth and photosynthesis, suppressed chlorophyll synthesis and nitrogen assimilation, and down-regulated genes associated with photosynthesis, Calvin cycle, and carbohydrate metabolism of N. yezoensis conchocelis filaments. However, N. yezoensis conchocelis filaments showed acclimation strategies under long-term OA, in terms of metabolic reorganization, prioritizing stress tolerance over growth. Further weighted gene co-expression network analysis (WGCNA) based on the metabolomic and transcriptomic results under long-term OA showed that the strategy was manifested by the accumulation of soluble sugars as osmolytes, lipid β-oxidation compensating for energy deficits, and H+ extrusion mediated via ABC transporters. This study suggested time-depended responses of N. yezoensis conchocelis filaments to OA, proving the pronounced negative effects of OA on N. yezoensis conchocelis filaments, revealing N. yezoensis conchocelis filaments could acclimate to long-term OA by resource reallocation. These findings provide new insight into the survival of N. yezoensis conchocelis filaments under OA, and facilitate the development of technologies and breeding strategies for improved acidification tolerance in N. yezoensis.

The Yangtze River Estuary is the terminal sink of terrestrial per- and polyfluoroalkyl substances (PFAS) from the Yangtze River, while the environmental fate characteristics of legacy and emerging PFAS around this region have rarely been discussed. Here, 24 targeted PFAS in seawater, sediments, suspended particulate matter (SPM), and plankton in the offshore region adjacent to this estuary were investigated. The three dominant PFAS in all phases were perfluorooctanoic acid (PFOA, 23.8-61.9%), perfluorobutanoic acid (PFBA, 23.6-42.8%), and perfluoro(2-methyl-3-oxahexanoic) acid (HFPO-DA, 6.1-12.1%), and perfluoro-1-butane sulfonamide (FBSA, 0.1-7.3%) was first detected. The horizontal distributions of PFAS were dependent on salinity and disturbed by multiple water masses, while the vertical variations could be explained by their different partitioning characteristics in the water-SPM-sediment system (partition coefficients, Log K_d and Log K_oc) and plankton (bioaccumulation factors, Log BAF). Although physical mixing was the major driver for PFAS settling (>83.7%), the absolute settling amount caused by the biological pump was still high (150.00-41994.65 ng m^-2 day^-1). More importantly, we found unexpected high Log K_d values of PFBA (2.24-4.55) and HFPO-DA (2.26-4.67), equal to PFOA (2.28-4.72), which brought concerns about their environmental persistence. Considering the increased detection of short-chain and emerging PFAS, more comprehensive environmental behaviors analysis is required urgently.