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Laboratory simulation of flocculation process and investigation of influencing important factors in estuaries using image processing 利用图像处理技术对河口絮凝过程的实验室模拟及影响因素的研究
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-30 DOI: 10.1016/j.ecss.2026.109739
Sajjad Fathi Ozanbolagh, Mohammad Hossein Niksokhan, Abdolreza Karbassi
Estuaries are intricate and fascinating aquatic environments where freshwater from rivers and streams converges with saline water from the ocean. This dynamic ecosystem is subjected to many factors, including salinity and other ions, which influence estuarine characteristics. One crucial process that impacts the size of suspended particles and the water quality in this environment is flocculation. The recent study explored and tested the flocculation process in river estuaries under conditions that resemble near real-life scenarios by image processing considering the various conditions of mixing in different parts of the hypothetical estuary and by examining a wide range of different salinity values, the concentration of suspended sediments and different volumes of saline water.
The study investigated three key factors: mixing processes, water salinity and the concentration of suspended substances. The research considered two broad perspectives for review: changes in salinity and changes in the volume of saline water mixed throughout the estuary. The findings indicate that the size of flocs in the estuary area fluctuates based on both salinity and river discharge, depending on the location along the hypothetical estuary. These changes are also influenced by the concentration of suspended sediments in the river water.
The statistical findings indicate that the smallest floc size occurs at a salinity of 12 g/l, while the largest floc size is observed at a salinity of 24 g/l. This maximum floc size is associated with a suspended sediment concentration of 50 mg/l and a volume of saline water equal to 1 L.
The results indicate that the maximum floc sizes predominantly occur within the salinity range of 18–24 g/l, with concentrations at both the minimum (50 mg/l) and maximum (200 mg/l) levels.
With changes in salinity along the estuary based on the different mixing conditions and different levels of suspended sediment concentration, the maximum size of the flocs varies.
河口是复杂而迷人的水生环境,来自河流和溪流的淡水与来自海洋的咸水汇合。这种动态生态系统受到许多因素的影响,包括盐度和其他离子,这些因素都会影响河口特征。在这种环境中,影响悬浮颗粒大小和水质的一个关键过程是絮凝。最近的研究通过图像处理,考虑了假设河口不同部分的各种混合条件,并通过检查大范围的不同盐度值、悬浮沉积物浓度和不同盐水体积,探索和测试了类似于接近现实场景的河口絮凝过程。研究考察了三个关键因素:混合过程、水盐度和悬浮物浓度。该研究考虑了两个广泛的观点:盐度的变化和整个河口混合盐水体积的变化。研究结果表明,河口区域絮凝体的大小随盐度和河流流量的变化而波动,这取决于假设河口的位置。这些变化还受到河水中悬浮沉积物浓度的影响。统计结果表明,矿化度为12 g/l时,絮凝体粒径最小,矿化度为24 g/l时,絮凝体粒径最大。此最大絮体大小与悬浮沉积物浓度为50 mg/l和盐水体积等于1 l有关。结果表明:最大絮凝体粒径主要发生在18 ~ 24 g/l的盐度范围内,最小浓度为50 mg/l,最大浓度为200 mg/l;不同混合条件和不同悬浮物浓度水平导致的河口沿岸盐度变化导致絮凝体的最大粒径变化。
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引用次数: 0
Seasonal comparison of primary productivity and microeukaryotic plankton community structure between two seagrass bed ecosystems in northern and southern China 南北方两个海草床生态系统初级生产力和微真核浮游生物群落结构的季节比较
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-24 DOI: 10.1016/j.ecss.2026.109732
Zhexuan Shi , Ziqi Liu , Jiahong Zhu, Zhi'en Liu, Hongwei Wang, Siyang Wu, Luyao Chen, Weifang Chen, Xin Lin
Seagrass beds, recognized as pivotal blue carbon ecosystems, are essential for mitigating climate change and sustaining coastal ecological functioning. While contributions to organic carbon storage from plant residues and terrestrial inputs in submerged seagrass meadows have been extensively studied, the temporal variations in the productivity and community structure of microeukaryotic plankton in the overlying water column remain underexplored, despite their critical role in primary productivity. Here, we compared the seasonal dynamics of gross primary productivity (GPP) and microeukaryotic plankton community structures between a temperate Swan Lake and a tropical Li'an Lagoon, both semi-closed seagrass bed ecosystems in China, revealing spatiotemporal heterogenous patterns and regulatory mechanisms. In the temperate Swan Lake, GPP increased gradually from spring to winter, whereas biomass chlorophyll a (Chla) remained consistently low across all seasons. In contrast, the tropical lagoon exhibited heterogeneous spatiotemporal dynamics of both Chla and GPP, driven by season and seagrass coverage. Regarding community composition, Stramenopiles, Alveolata, unclassified Eukaryota, Chlorophyta and Cryptophyta, collectively accounted for over 90 % of total abundance, exhibiting significant seasonal and spatial dynamics in two regions, respectively. We further found that the microeukaryotic plankton community diversity and assembly mechanism were primarily driven by stochastic processes, ecological drift and homogenizing dispersal. These findings underscore the crucial role of seagrass in regulating microorganism community assembly and ecosystem resilience, providing a scientific basis for developing conservation strategies for coastal seagrass beds sensitive to human activities.
海草床被认为是关键的蓝碳生态系统,对减缓气候变化和维持沿海生态功能至关重要。虽然植物残体和陆地输入对沉水海草草甸有机碳储存的贡献已经得到了广泛的研究,但尽管浮游微真核生物在初级生产力中起着关键作用,但其生产力和群落结构的时间变化仍未得到充分探索。本文比较了中国温带天鹅湖和热带黎安湖两种半封闭式海草床生态系统的总初级生产力(GPP)和微真核浮游生物群落结构的季节动态,揭示了它们的时空异质性格局和调控机制。在温带天鹅湖,GPP从春季到冬季逐渐增加,而生物量叶绿素a (Chla)在所有季节都保持较低水平。热带泻湖Chla和GPP在季节和海草覆盖的驱动下呈现出异质性的时空动态。群落组成方面,层门、肺泡门、未分类真核、绿藻门和隐藻门占总丰度的90 %以上,在两个区域分别表现出明显的季节和空间动态。我们进一步发现,微真核浮游生物群落多样性和组装机制主要受随机过程、生态漂变和均质扩散驱动。这些发现强调了海草在调节微生物群落聚集和生态系统恢复力方面的重要作用,为制定人类活动敏感的沿海海草床保护策略提供了科学依据。
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引用次数: 0
Mesh size efficiency in estuarine benthos sampling: impact on community composition and the performance of ecological indicators in the Amazon region 河口底栖生物取样的网目尺寸效率:对群落组成和生态指标表现的影响
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-23 DOI: 10.1016/j.ecss.2026.109731
Rafael Anaisce das Chagas , Mara Rúbia Ferreira Barros , Weverton John Pinheiro dos Santos , Raphael Ligeiro
In this study, we performed an analysis of the sampling efficiency of different mesh sizes in the sampling of estuarine benthic communities. Sampling was carried out at four points in the Primavera River estuary (Eastern Amazon), in September 2020, using four quadrants (1 m2 each) at each point, arranged in two parallel transects (riverbank and mangrove forest) located within the intertidal region. In the laboratory, we sorted the samples using meshes with openings of 0.5 mm, 1.0 mm and 2.0 mm and identified them at the lowest possible taxonomic level. The results showed that the retention efficiency of the 1.0 mm and 2.0 mm meshes were similar, both with smaller abundance values than obtained by the 0.5 mm mesh size. The difference found in species richness was mainly due to the presence of some taxa found only in the finer mesh, such as ostracods, foraminifera and nematodes. Furthermore, the ecological responses using the ecological indicators did not show differences between the mesh sizes evaluated. We concluded that the use of a larger mesh (2.0 mm) has proven to be effective in studies that aim at the characterization of the ecological condition of sites or investigations of the relationships between organisms and their habitat. The use of the finer mesh (0.5 mm), with a greater abundance of individuals and species richness, should be reserved only for more rigorous diversity surveys, since the loss of information in relation to the larger mesh was not expressive.
在本研究中,我们对河口底栖生物群落采样中不同网目尺寸的采样效率进行了分析。2020年9月,在Primavera河河口(亚马逊东部)的四个点进行了采样,每个点使用四个象限(每个1 m2),分布在潮间带区内的两个平行样带(河岸和红树林)中。在实验室中,我们使用开口分别为0.5 mm、1.0 mm和2.0 mm的网目对样品进行分类,并在尽可能低的分类水平上进行鉴定。结果表明,1.0 mm和2.0 mm网目的截留效率相似,丰度值均小于0.5 mm网目的截留效率。物种丰富度的差异主要是由于介形虫、有孔虫和线虫等仅存在于较细孔的分类群。此外,使用生态指标的生态响应在评估的网目大小之间没有差异。我们的结论是,使用更大的网格(2.0 mm)已被证明是有效的,旨在研究地点的生态条件特征或调查生物与其栖息地之间的关系。使用更细的网目(0.5 mm),具有更丰富的个体和物种丰富度,应该只用于更严格的多样性调查,因为与更大的网目相关的信息损失不具有表达性。
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引用次数: 0
Rapid macrobenthos colonization of newly created intertidal habitat in the Hedwige-Prosper Polder managed realignment site (Scheldt estuary, Belgium, the Netherlands) 大型底栖动物在海德威格-普洛斯波尔德管理的重新调整地点新创建的潮间带栖息地的快速殖民化(比利时,荷兰的斯海尔特河口)
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-22 DOI: 10.1016/j.ecss.2026.109730
Tom Van den Neucker , Roy Münstermann , Stijn Baeten, Tim van den Broeck, Robrecht Debbaut, Tom Maris, Jonas Schoelynck
Over the last 25 years, a series of flood control areas and managed realignment sites have been established along the entire salinity gradient of the Scheldt estuary in Belgium and the Netherlands, which serve both as flood protection measures and to compensate for the loss of intertidal mudflats and marshes caused by anthropogenic perturbations. In October 2022, the Hedwige-Prosper Polder managed realignment site became operational, consisting of the former Prosper and Hedwige Polders and the Sieperda Marsh. We examined the macrobenthos colonization of the Hedwige-Prosper managed realignment site during the first year after tidal restoration. We also investigated the driving abiotic factors behind the macrobenthos community development. Macrobenthos samples, sediment samples and elevation measurements were collected at ten locations covering the entire elevation gradient of the site. Multivariate statistics were used to evaluate the effect of season on macrobenthos species composition, to investigate the relationship between biotic and abiotic variables and to assess the effect of abiotic variables on macrobenthos density. Macrobenthos colonization was rapid. The number of taxa increased sharply between spring and autumn. A total of 28 macroinvertebrate taxa were found 11 months after realignment, of which 21 occurred on the newly created mudflat in the former Prosper and Hedwige Polders. Spatial variation in the macrobenthos community was explained by differences in inundation frequency. Our results indicate that the macrobenthos of the newly created mudflat in the Hedwige-Prosper Polder converges to benthos communities found on natural mudflats in the mesohaline and polyhaline zones of the Scheldt estuary.
在过去的25年里,在比利时和荷兰的斯海尔德河口的整个盐度梯度上建立了一系列的洪水控制区和管理的重新调整地点,这既是防洪措施,也是补偿因人为扰动造成的潮间带泥滩和沼泽的损失。2022年10月,Hedwige-Prosper Polder管理的重新调整地点开始运营,包括前Prosper和Hedwige Polders以及Sieperda Marsh。在潮汐恢复后的第一年,我们研究了Hedwige-Prosper管理的调整地点的大型底栖动物的殖民。研究了大型底栖动物群落发展的非生物驱动因素。在覆盖整个高程梯度的10个地点采集了大型底栖动物样本、沉积物样本和高程测量数据。采用多元统计方法评价季节对大型底栖动物物种组成的影响,探讨生物变量与非生物变量的关系,评价非生物变量对大型底栖动物密度的影响。大型底栖动物定植迅速。春秋两季分类群数量急剧增加。调整后11个月共发现28个大型无脊椎动物类群,其中21个发生在原Prosper和Hedwige圩区新形成的泥滩上。大型底栖动物群落的空间差异可以用淹没频率的差异来解释。我们的研究结果表明,在Hedwige-Prosper圩区新形成的泥滩上,大型底栖动物群落与Scheldt河口中盐带和多盐带的天然泥滩上的底栖动物群落趋同。
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引用次数: 0
Impact of an estuarine dam on sediment distribution and accumulation in the Geum Estuary, South Korea 韩国锦江河口坝对泥沙分布和堆积的影响
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-21 DOI: 10.1016/j.ecss.2026.109717
Timothy M. Dellapenna , Guan-hong Lee , Jonathan Rogers , Peng Lin , Joshua Alarcon , Jongwi Chang
The Geum Estuary, located on the west coast of South Korea, provides a compelling case study of estuarine transformation under intensive anthropogenic modification. Following the construction of the Geum Estuarine Dam in 1994, the estuary has undergone marked changes in hydrodynamics, sediment transport pathways, and depositional environments. To quantify these changes, a suite of vibracores was collected upstream of the dam, within the inner estuary, across adjacent tidal flats, and on the inner continental shelf. Grain size distribution, sediment geochemistry, and radionuclide-based geochronologies (210Pb and 239+240Pu) were used to reconstruct depositional trends and assess sediment retention dynamics. The results demonstrate a pronounced shift from sand-to mud-dominated environments downstream of the dam, with sedimentation rates reaching 6–8 cm/yr−1. In contrast, formerly mud-rich offshore zones now exhibit sandier stratigraphy and reduced accumulation rates, while coarse sediments continue to dominate upstream of the dam. These patterns are consistent with the ∼54 % reduction in tidal prism and the dam's top-gate discharge design, which restricts bottom flows and promotes trapping of suspended sediment within the estuary. Seasonal processes such as strain-induced periodic stratification and episodic dam releases further reinforce sediment convergence in the inner estuary. This study highlights the long-term legacy effects of river regulation on estuarine sediment dynamics and pollutant accumulation. The findings have broader implications for the management of dammed estuaries in monsoon-influenced regions. The Geum Estuary serves as a critical reference for evaluating sedimentological consequences of human interventions in estuarine systems globally.
位于韩国西海岸的锦河口,是人类活动影响下河口变化的一个引人注目的研究案例。自1994年修建锦河口大坝以来,河口的水动力、输沙途径、沉积环境都发生了明显的变化。为了量化这些变化,在大坝上游、内河口、邻近的潮滩和内大陆架上收集了一套振动核。利用颗粒粒度分布、沉积物地球化学和放射性核素年代学(210Pb和239+240Pu)重建沉积趋势并评估沉积物保持动力学。结果表明,大坝下游的环境从以沙为主转向以泥为主,沉积速率达到6-8 cm/yr - 1。相比之下,以前富含泥土的近海地区现在呈现砂质地层,堆积速率降低,而粗质沉积物继续在大坝上游占主导地位。这些模式与潮汐棱镜减少54%和大坝顶闸排放设计相一致,后者限制了底部水流并促进了河口内悬浮沉积物的捕获。季节性过程,如应变引起的周期性分层和偶发性水坝释放,进一步加强了河口内沉积物的收敛。本研究强调了河流调控对河口泥沙动态和污染物积累的长期遗留效应。这一发现对受季风影响地区的河口坝管理具有更广泛的意义。锦河口是评价人类干预对全球河口系统的沉积学影响的重要参考。
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引用次数: 0
Intraseasonal variation of sea surface temperature and its primary mechanism in Bohai Sea 渤海海表温度的季节内变化及其主要机制
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-20 DOI: 10.1016/j.ecss.2026.109718
Jia Shi , Zhiliang Liu , Yunlong Lu , Yongliang Zhang , Xiao Chen , Zuozuo Ma
Sea surface temperature (SST) variability on intraseasonal timescales (10–90 days) significantly influences regional weather and marine ecosystems. However, intraseasonal SST variability in the Bohai Sea remains poorly understood. Based on high-resolution satellite SST data and ERA5 reanalysis data, this paper systematically examines the spatiotemporal characteristics and underlying mechanisms of intraseasonal SST variability in the Bohai Sea. Spectral analysis identifies two significant intraseasonal oscillation (ISO) periods of Bohai Sea SST: a shorter-period oscillation (30–50 days, ISO30–50) and a longer-period oscillation (60–90 days, ISO60–90). The ISO30–50 dominates in summer and is primarily driven by shortwave radiation anomalies that lead SST variations by 2–7 days. The ISO60–90 occurs mainly in autumn and winter and is predominantly controlled by turbulent heat fluxes (primarily latent and sensible heat fluxes), whose anomalies precede SST changes by 11–14 days. Longwave radiation acts as different feedback mechanism in two periods. In the ISO60–90 band, upward longwave radiation varies almost simultaneously with SST. In contrast, in the ISO30–50 band, downward longwave radiation may lead SST in an anti-phase manner under certain atmospheric conditions. Spatially, the ISO30–50 concentrates in shallow coastal bays, whereas the ISO60–90 extends across larger offshore areas. Notably, the spatial patterns of ISOs do not fully align with the heat flux variability, suggesting that oceanic circulation structures may play a crucial role in regulating the spatial heterogeneity of intraseasonal SST oscillations. These findings advance the mechanistic understanding of Bohai Sea SST variability and provide insights for predicting regional weather and managing nearshore ecological environments.
海表温度(SST)在季节内时间尺度(10-90天)上的变化显著影响区域天气和海洋生态系统。然而,对渤海海温的季节内变化仍知之甚少。基于高分辨率卫星海温资料和ERA5再分析资料,系统探讨了渤海海温季节内变化的时空特征及其机制。谱分析表明,渤海海表温度存在两个显著的季节内振荡周期:短周期振荡(30-50 d, ISO30-50)和长周期振荡(60-90 d, ISO60-90)。ISO30-50在夏季占主导地位,主要由短波辐射异常驱动,导致海温变化2-7天。ISO60-90主要发生在秋季和冬季,主要受湍流热通量(主要是潜热通量和感热通量)控制,其异常比海温变化早11-14天。长波辐射在两个周期中表现为不同的反馈机制。在ISO60-90波段,向上的长波辐射几乎与海温同步变化。而在ISO30-50波段,在一定的大气条件下,向下的长波辐射可能以反相方式引导海温。在空间上,ISO30-50集中在浅海沿岸海湾,而ISO60-90则延伸到更大的近海地区。值得注意的是,ISOs的空间格局与热通量变化并不完全一致,这表明海洋环流结构可能在调节季节内海温振荡的空间异质性中起关键作用。这些发现有助于进一步认识渤海海温变率的机理,为区域天气预报和近岸生态环境管理提供参考。
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引用次数: 0
Long-term changes in the Adriatic Sea (1971–2023): river influence, climate impacts, and biogeochemical shifts in coastal bottom waters 亚得里亚海的长期变化(1971-2023):河流影响、气候影响和沿海底部水域的生物地球化学变化
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-20 DOI: 10.1016/j.ecss.2026.109722
Teresa Sani , Alessandra Campanelli , Mauro Marini , Stefano Goffredo , Federica Grilli
This study analyses long-term (1971–2023) trends in physical (temperature and salinity) and biogeochemical (chlorophyll-a and nitrate concentration) properties of bottom coastal waters in the Western Adriatic Sea. Results reveal complex patterns driven by a combination of regional hydrological shifts and broader climate change impacts. The basin was divided into North and Central-South sub-basins, focusing on winter and summer data. Over the last 53 years, Po River flow has progressively decreased especially during summer, altering hydrography and nutrient dynamics. Marked regional and seasonal divergences were observed. The North Adriatic showed summer warming (+1.05 % yr−1), slight winter cooling (−0.27 % yr−1), and decreased salinity in winter with a slight increase in summer. In contrast, the Central-South Adriatic exhibited stronger winter warming (+0.43 % yr−1), weaker summer warming (+0.08 % yr−1), increased salinity in winter and a decline in summer. Biogeochemical trends revealed strong regional and seasonal contrasts in chlorophyll-a and nitrate concentrations, with declining summer chlorophyll-a across the basin and decreases in both chlorophyll-a and nitrate in the Central-South Adriatic, consistent with a long-term, phosphorus-driven reduction in trophic conditions. This research helps to fill a critical knowledge gap concerning increasingly vulnerable and impacted coastal and bottom environments, underscoring the importance of sustained basin-wide monitoring to ensure uniform spatial and temporal coverage.
本研究分析了西亚得里亚海底岸水体的物理(温度和盐度)和生物地球化学(叶绿素-a和硝酸盐浓度)特性的长期(1971-2023)趋势。结果揭示了由区域水文变化和更广泛的气候变化影响共同驱动的复杂模式。以冬季和夏季资料为重点,将盆地划分为北部和中南部两个子盆地。在过去的53年里,波河流量逐渐减少,特别是在夏季,改变了水文和营养动态。观察到明显的区域和季节差异。北亚得里亚海夏季增温(+ 1.05% yr - 1),冬季轻微降温(- 0.27% yr - 1),冬季盐度下降,夏季盐度略有上升。中南部亚得里亚海冬季增温较强(+ 0.43% yr - 1),夏季增温较弱(+ 0.08% yr - 1),冬季盐度升高,夏季盐度下降。生物地球化学趋势揭示了叶绿素-a和硝酸盐浓度的强烈区域和季节差异,夏季整个盆地的叶绿素-a下降,中南部亚得里亚海的叶绿素-a和硝酸盐均下降,这与长期磷驱动的营养条件减少相一致。这项研究有助于填补关于日益脆弱和受影响的沿海和底部环境的关键知识空白,强调了持续的全流域监测以确保统一的时空覆盖的重要性。
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引用次数: 0
Machine learning-based detection of mangrove dynamics in a subtropical bay: reasons and outcomes 基于机器学习的亚热带海湾红树林动态检测:原因和结果
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-19 DOI: 10.1016/j.ecss.2026.109719
Xiaowen Xie , Zhijun Dai , Riming Wang , Tianliang Wu , Baoqing Hu , Xixing Liang
Mangrove forests constitute one of the most carbon-dense ecosystems in tropical and subtropical intertidal zones, providing significant ecological and economic benefits worldwide. Nevertheless, these vital ecosystems have experienced substantial degradation in recent decades, primarily attributable to escalating anthropogenic pressures and rising sea levels. Here, this study employed remote sensing imagery (1987–2023) and machine learning to examine mangrove forest dynamics in Fangcheng Bay (FCB), a subtropical bay in China's Beibu Gulf. Our analysis demonstrated a remarkable 182.38 % expansion in FCB's mangrove coverage over the 36-year period (1987–2023), with total area increasing from 233.19 ha to 658.49 ha. The West Bay (WB) and East Bay (EB) exhibited respective increases of 52.98 % and 274.47 %. Meanwhile, landward mangroves declined while seaward expansion occurred at an average shoreline progression rate of 1.28 m/yr. Furtherly, our analysis indicates that neither sea level rise nor estuarine declining suspended sediment concentration significantly influenced mangrove expansion. Tidal current-driven sediment deposition created optimal growth conditions by continuously replenishing mangrove tidal flats. These findings elucidate the drivers and patterns of FCB's mangrove dynamics amid rapid urbanization, offering critical implications for global mangrove conservation in comparable bay systems.
红树林是热带和亚热带潮间带碳密度最高的生态系统之一,在世界范围内提供了巨大的生态和经济效益。然而,近几十年来,这些重要的生态系统经历了严重退化,主要原因是人为压力不断加剧和海平面上升。在这里,本研究利用遥感图像(1987-2023)和机器学习研究了中国北部湾的亚热带海湾方城湾(FCB)的红树林动态。我们的分析表明,在1987-2023年的36年期间,FCB红树林覆盖面积显著增加了182.38%,总面积从233.19 ha增加到658.49 ha。西湾(WB)和东湾(EB)分别增长了52.98%和274.47%。与此同时,向陆地的红树林减少,而向海洋的扩张以平均1.28 m/年的海岸线推进率发生。此外,我们的分析表明,海平面上升和河口悬沙浓度下降都没有显著影响红树林的扩张。潮汐驱动的沉积物沉积通过不断补充红树林潮滩创造了最佳的生长条件。这些发现阐明了快速城市化中FCB红树林动态的驱动因素和模式,为可比海湾系统的全球红树林保护提供了重要意义。
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引用次数: 0
Human activity intensifies land subsidence in the Yellow River Delta 人类活动加剧了黄河三角洲的地面沉降
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-18 DOI: 10.1016/j.ecss.2026.109721
Hui Xu , De Wang , Rongrong Ning , Xiaoyong Li , Xinpeng Tian , Xiaoli Bi , Zixiang Zhou , Yongwei Zhang
The intensification of human activity in the 21st century has led to a rapid land subsidence along the Yellow River Delta coast, which threatens the region's future sustainable development. This study uses Sentinel-1A imagery acquired between April 2017 and June 2024 and the SBAS-InSAR method to obtain subsidence information for the Yellow River Delta. We quantified the natural and human factors influencing subsidence and explored the relationship between brine mining, soft soil thickness, the seasonal groundwater level fluctuation, and subsidence. The main results are as follows. The SBAS-InSAR measurements exhibited a high inversion accuracy, with an average error of ±6.9 mm/yr and a median error of ±8.6 mm/yr. The four major subsidence zones are all located in the brine mining area, with the subsidence rate reaching 325 mm/yr in the peak zone, indicating brine extraction is the most representative of human activity in the Yellow River Delta and plays a dominant role in subsidence. The driving factors influencing subsidence are ordered as salt fields distribution, nearshore distance, and GDP, with corresponding q-values (explanatory power) of 0.21, 0.14, and 0.07, respectively. Precipitation-driven fluctuations in shallow groundwater levels can affect ground deformation in most regions except the brine extraction area. Our findings can provide management support for subsidence control and flood prevention in the Yellow River Delta.
21世纪以来,人类活动的加剧导致黄河三角洲沿海地区地面快速沉降,威胁着该地区未来的可持续发展。本研究利用2017年4月至2024年6月期间获取的Sentinel-1A图像和SBAS-InSAR方法获取黄河三角洲的沉降信息。量化了影响沉陷的自然因素和人为因素,探讨了卤水开采、软土厚度、季节性地下水位波动与沉陷的关系。主要结果如下:SBAS-InSAR测量具有较高的反演精度,平均误差为±6.9 mm/yr,中位误差为±8.6 mm/yr。4个主要沉陷带均位于卤水矿区,峰值区沉陷速率达325 mm/yr,说明黄河三角洲地区最具人类活动代表性的是抽卤,对沉陷起主导作用。影响沉降的驱动因素依次为盐田分布、近岸距离、GDP,其q值(解释能力)分别为0.21、0.14、0.07。降水驱动的浅层地下水位波动可以影响除盐水提取区以外的大部分地区的地面变形。研究结果可为黄河三角洲地区的沉降控制和防洪提供管理支持。
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引用次数: 0
Century-long coral evidence of climate and anthropogenic influences on tropical coastal phosphorus cycling in the northern South China Sea 南海北部热带沿海磷循环受气候和人为影响的百年珊瑚证据
IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Pub Date : 2026-01-17 DOI: 10.1016/j.ecss.2026.109720
Ning Guo , Wei Jiang , Kefu Yu , Jian-xin Zhao , Yinxian Song , Yue-xing Feng , Chunmei Feng
Phosphorus (P) is a critical and scarce nutrient in marine ecosystems, playing a vital role in sustaining primary productivity. Its dynamic variations are closely linked to coastal anthropogenic activities and climate change. However, due to the lack of long-term continuous observational data, our understanding of the evolution patterns of coastal nutrients at interannual to centennial scales remains limited. Coral skeletal phosphorus-to-calcium ratio (P/Ca) has been demonstrated to be a robust proxy for reconstructing long-term phosphate variations in seawater. This study utilized P/Ca ratios in Porites lutea coral from the Luhuitou fringing reef of Hainan Island to reconstruct the historical variations of dissolved inorganic phosphorus (DIP) in surface seawater since 1870. The results reveal that coral P/Ca ratios in the Sanya coastal waters are jointly regulated by terrestrial inputs and upwelling processes. Specifically, P fertilizer application in agricultural activities has significantly increased terrestrial P loading, which is subsequently transported to coastal waters via submarine groundwater discharge (SGD). Crucially, El Niño-Southern Oscillation (ENSO)-driven regional hydrothermal conditions play a pivotal regulatory role in this process. Precipitation provides the transport momentum, while the anomalous high temperatures during El Niño years significantly accelerate chemical weathering, thereby greatly enhancing the P transport flux. Furthermore, against the background of long-term climate warming, this temperature-dominated weathering and transport mechanism is intensifying. The ENSO-modulated upwelling transports P-enriched deep water to the surface, creating a cumulative effect with anthropogenic P sources that collectively enhances marine primary productivity. Notably, the decline in live coral coverage of the Luhuitou fringing reef occurred prior to the marked rise in the coral P/Ca ratio, indicating that elevated DIP concentrations in seawater are not the primary driver of ecological degradation in this reef. This study not only confirms the unique value of coral geochemical proxies in deciphering long-term nutrient dynamics, but also highlights that the ongoing intensification of soil P weathering-transport processes in tropical regions under anthropogenic climate warming may pose potential ecological risks. These findings provide critical scientific supports for integrated coastal zone management.
磷是海洋生态系统中重要而稀缺的营养物质,对维持初级生产力起着至关重要的作用。其动态变化与沿海人为活动和气候变化密切相关。然而,由于缺乏长期的连续观测资料,我们对沿海营养物在年际到百年尺度上的演变模式的认识仍然有限。珊瑚骨骼磷钙比(P/Ca)已被证明是重建海水中长期磷酸盐变化的有力代理。本研究利用海南岛鹿水头边缘礁Porites lutea珊瑚的P/Ca比值,重建了1870年以来表层海水中溶解无机磷(DIP)的历史变化。结果表明,三亚近岸海域珊瑚磷钙比受陆地输入和上升流共同调节。具体而言,在农业活动中施用磷肥显著增加了陆地磷负荷,随后通过海底地下水排放(SGD)将其输送到沿海水域。至关重要的是,El Niño-Southern涛动(ENSO)驱动的区域热液条件在这一过程中起着关键的调节作用。降水提供了输运动量,而El Niño年的异常高温显著加速了化学风化,从而大大增强了P输运通量。此外,在长期气候变暖的背景下,这种以温度为主导的风化运输机制正在加剧。enso调制的上升流将富含P的深水输送到地表,与人为P源形成累积效应,共同提高海洋初级生产力。值得注意的是,鹿回头珊瑚礁活珊瑚覆盖率下降发生在珊瑚P/Ca比值显著上升之前,表明海水中DIP浓度升高不是该珊瑚礁生态退化的主要驱动因素。本研究不仅证实了珊瑚地球化学指标在破译长期营养动态方面的独特价值,而且强调了人为气候变暖下热带地区土壤P风化运输过程的持续加剧可能带来潜在的生态风险。这些发现为海岸带综合管理提供了重要的科学依据。
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引用次数: 0
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Estuarine Coastal and Shelf Science
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