社会-生态综合视角下海岸带生态监管框架与应用——以深圳为例

海岸带作为海洋与陆地两大生态系统的连接与桥梁，既是国民经济、社会发展的重要区域与战略中心，也是生态环境破坏和污染的热点区域。以往针对海岸带区域开展的城市化对生态环境的影响研究，主要利用30 m空间分辨率的Landsat数据分析城市扩张对自然生态系统的侵占，如自然用地减少、景观异质性降低、填海造陆速度变快等，而针对污染产业、人类活动等引起的河口水质污染、水温异常、自然岸线退化等复杂生态环境问题关注不足，难以满足陆海统筹管理、综合防治的需求。因此，研究围绕海岸带面临的主要问题，面向海岸带生态环境综合管制，构建了“问题识别-格局量化-地面调查-生态监管”的综合框架，通过明确生态环境问题，量化社会-生态格局，开展实地调查，制定生态监管目标和策略。通过融合高分影像、兴趣点、道路等多源异构数据并结合地面调查，准确识别影响生态环境的社会-生态格局因子，实现空间显性的生态监管。进一步以深圳为典型案例，探讨该概念框架的应用，将深圳市海岸带划分为了四类共980个生态监管单元，其中包括153个优先保护单元，主要为分布在海岸带东部的林地，7个生态风险较大的核心管控单元，597个几乎分布在海岸带西部的重点管控单...     

海岸带综合管理及其研究进展

协调海岸带区域综合承载力与经济社会可持续发展的关系,加强和实施海岸带综合管理(ICZM)和可持续发展战略是当今政府与社会各界关注的热点。海岸带综合管理需要多部门协作配合,综合运用社会、经济、环境、法律等多方面技术实现科学的海岸带管理。根据当前发展趋势,海岸带综合管理进展可归纳为:人文与自然过程变化与海岸带响应;基于不同目标的海岸带规划;海岸带综合管理的评价;新技术与方法应用;利益冲突与关系协调;生态关键区保护与管理;政策与法规制定与调整。在综述海岸带综合管理的发展历程的基础上,探讨了海岸带综合管理的展望。     

全球变化下海岸带微生物生态研究进展

海岸带地区是元素循环最活跃的自然区域之一,微生物作为地球元素循环的主要驱动者,对该区域生态系统中物质转化与能量流动起着至关重要的作用。本文从典型海岸带生态系统：海岸带湿地、海草床与海藻森林、近岸水体出发,围绕微生物参与的碳、氮循环过程以及其中的温室气体排放情况,综述了在全球气候变化与人为活动干扰的作用下,海岸带地区的微生物群落对外界环境变化的响应机制以及生态功能维持机制,最后对海岸带系统中微生物生态研究进行了初步的展望。     

基于土地利用变化和生态系统服务的海岸带生态安全综合评价——以胶州湾为例

以土地利用为主的陆域开发活动能改变近海环境质量,并影响和改变原有海岸带生态系统服务功能的供给模式,对海岸带生态安全产生一定的负面影响.目前在海岸带生态系统研究领域较多采用陆地生态系统研究模式,未能真正体现海岸带作为海陆结合的独立的环境体系的特点,并缺乏对陆域活动驱动与生态系统服务功能响应和生态安全实现之间复杂关系的科学解释.本研究基于海岸带生态系统服务的空间异质性和流动性特点,以“土地利用变化(LUCC)-生态系统服务(ES)-生态系统安全”为研究主线,构建海岸带生态安全评价模型,探讨以土地覆被变化为主的陆域活动对海岸带生态系统服务功能和区域生态安全的影响机理及其时空变异规律.从模型的评价结果上看,作为生态安全系统中主要压力表征的胶州湾陆域土地利用变化,与相应海域内的生态系统服务状况和生态安全状态呈现出一定的相关性和趋势性.随着环胶州湾地区城市化进程中大量用地流转为城乡建设用地,胶州湾中相应海域的生态系统服务状态下降,进而带来该海域生态安全状态恶化.本文所提出的基于压力-状态-响应(PSR)框架的海陆结合的生态安全评价模型,以探讨陆域活动对海岸带生态系统服务功能和区域生态安全的影响及其时空变异规律为目的,可以克服目前研究中只关注陆域部分而忽视陆域活动与海域部分之间的联系和相互影响的缺陷,对海岸带生态安全评价研究具有一定的改进作用.     

粤港澳大湾区城镇化对海岸线与海岸带的影响

海岸带以丰富的自然资源与优越的地理位置成为城镇化的关键地带。基于Google Earth平台2001、2010、2018年高分影像识别分析了粤港澳大湾区快速城镇化过程中海岸线长度的变化,并分析了大湾区海岸带土地利用/土地覆被(land use/land cover, LULC)变化,以及定量解析了大湾区滨海城市城镇化与海岸带城镇用地的关联关系。结果表明:(1)2001—2018年,粤港澳大湾区海岸线总长度净增加32.24 km,但自然岸线人工化问题突出,自然岸线共减少187.67 km,人工岸线共增加219.91 km;(2)海岸带(海岸线向陆侧5 km缓冲区) LULC组成以耕地为主,但城镇用地对耕地的侵占问题突出,2001—2018年,耕地面积减少347.58 km~2,城镇用地面积增加588.33 km~2;(3)2001—2018年,滨海城市土地城镇化与海岸带城镇用地增长呈显著相关,并且滨海城市土地城镇化对海岸带城镇用地增加的影响在加强(2001—2010年和2010—2018年贡献率分别为43.7%和68.51%)。研究结果可对粤港澳大湾区海岸带保护、修复以及土地利用规划管理...     

厦门市土地利用变化下的生态敏感性

当前,城市化与全球变化背景叠加,海岸带生态系统发生了巨大的变化,沿海城市在全球变化下的脆弱性、敏感性与适应能力等问题已经成为政府和科学界关注的重要问题.土地利用变化是导致生态系统敏感性的重要因素之一.以厦门市作为沿海城市的典型代表,对近20 a土地利用变化下的生态敏感性进行系统研究.分析了城市建设用地扩张、围填海等主要土地利用活动对生态敏感性的影响机制;其次建立土地利用变化下的生态敏感性指数,并分析其变化过程;最后通过ArcGIS图层叠加计算功能,获得生态敏感性空间分布状况.结果表明:1987-2007年厦门市城市建设用地面积由1987年的67.48 km2,增加为2007年的308.21 km2,扩张了4.57倍,主要为蚕食农业用地和林地而来;海岸线长度由1987年的290.19 km,增加为1992年的343.23 km,而后减小为2007年的299.93 km,围垦养殖活动使得岸线变得曲折,填海造地活动导致岸线变得平滑.厦门市土地利用强度由1987年的2.44逐年增加为2007年的2.52,生态系统服务价值总体呈现减小的趋势,由1987年的7.39×109元减少到2007年的7.02× 109元,土地利用强度与生态系统服务价值呈现负相关关系.土地利用变化下的生态敏感性指数由1992年的1.50增加为1997年的4.94,而后减小为2002年的4.12,再增加为2007年的4.47.整体而言,近20a来厦门市生态系统对土地利用变化的敏感性灵敏响应程度不很剧烈,生态敏感性高的区域主要位于沿海区域.     

粤港澳大湾区海岸带生态系统保护和修复策略

粤港澳大湾区是我国海岸带高强度开发区域,面临着生态环境质量不高、生态系统受损严重的压力,开展海岸带生态系统保护修复是绿色湾区发展的必然需求。在分析大湾区海岸带基底、生态环境现状及问题的基础上,提出大湾区海岸带生态系统保护修复规划的策略,从以下5个方面构筑粤港澳大湾区海岸带生态系统保护修复规划的体系：一是从陆海污染统筹治理来恢复海域生物生存环境;二是从自然岸线保护、自然保护地体系重构与规范化建设、珍稀濒危物种栖息地保护来加强海岸带生态的保护;三是通过岸线生态修复、典型滨海湿地生态系统（红树林、珊瑚礁、海草床）修复、受损海岛生态修复来构筑生态安全屏障;四是从海堤生态化改造与建设、沿海防护林体系建设和海岸带综合防护工程建设来促进生态减灾协同增效;五是打造智慧海岸带管理服务平台来保障海洋命运共同体健康发展。本研究提出大湾区海岸带生态保护修复策略,期望为大湾区生态建设和环境保护提供参考。     

海岸带城市生态承载力综合评价——以连云港市为例

海岸带是人类聚居和海洋资源开发利用的重点区域。海岸带城市综合生态承载力体现了海岸带生态系统对人类社会经济活动的承受能力,是判断海岸带城市生态系统健康程度和制定海岸带环境管理政策的重要依据。基于"压力(P)-状态(S)-响应(R)"概念模型,以连云港市为例,构建海岸带综合生态承载力评价指标体系,并对2005—2014年间连云港市的综合生态承载力进行评价。结果显示:连云港市海岸带综合生态承载力呈现逻辑斯蒂式波动上升趋势,2005—2007年处于超载状态,2008—2011年基本处于平衡状态,2012年后处于可载状态。对影响承载力的主要因素进行贡献度分析的结果表明:负向指标中,海岸带环境压力大于人口压力;正向指标中,海岸带经济发展水平及科技支撑条件的贡献呈上升趋势,海岸带可利用资源波动下降。结合相关分析和因子分析,得出海岸带环境压力、科技支撑条件及经济发展水平是制约综合承载力的关键因素。研究结果对海岸带地区环境管理及可持续发展政策制定具有重要意义。     

基于生态系统服务价值的莱州湾-黄河三角洲海岸带区域生态连通性评价

基于最小累积费用模型(MCR)和生态连接度指数(ECI),对莱州湾-黄河三角洲海岸带区域的生态连通性进行综合评价。结果显示:(1)莱州湾-黄河三角洲海岸带区域生态连通性存在明显的陆海梯度变化特征,以海岸滩涂地带为中心向两侧辐射呈条带状递减;(2)2000—2015年生态连通性指数整体呈现明显的下降趋势,下降幅度达12.69%;城市化和交通等基础设施建设使区域人工障碍物集聚化和扩张趋势明显,加剧陆域生态景观的破碎化和孤岛化趋势,从而导致生态系统服务功能退化、生态连通性降低;(3)莱州湾-黄河三角洲海岸带区域生态连通性整体处于较低水平,极低连通性和低连通性分布面积占比最大,较高连通性区域呈现向次一级或更低等级连通性转变的趋势。不同等级生态连通性分布区域的转移变化反映了人类活动和自然因素双重干扰下莱州湾-黄河三角洲海岸带生态系统格局及其物质、能量、生物、信息流等的变化规律。研究将为莱州湾-黄河三角洲生态系统保护与海岸带综合管理提供相关科学参考。     

城市生态保护红线划定与管理——以澳门特别行政区为例

我国澳门特别行政区是世界上人口密度最高的地区之一,人地关系紧张。随着城市和经济的发展,人类空间与生态空间失调,城市生态和人居环境问题不断加剧。在建设美丽湾区、美丽澳门和人们对美好人居环境需求的背景下,通过划定城市生态保护红线以控制和维持现有重要功能生态空间,保护和改善高敏感生态空间,维护区域生态安全显得尤为重要。基于对澳门陆域生态系统调查,结合城市和自然资源特征,从生态系统服务功能、生态系统敏感性、生物多样性分布以及现有生态保护区四个方面构建了城市生态保护红线划定方法框架,选取并评估水源涵养、雨洪调节、热岛调节、土壤保持、海岸带防护五类调节服务和生态系统服务中的休闲游憩的空间格局,水土流失敏感性和海岸带风暴潮敏感性两种生态敏感性的分布,并综合澳门具有保育价值生物的栖息地分布和现有保护区范围进行了城市生态保护红线的划定。研究结果显示,澳门城市生态保护红线区域总面积6.71km²,占研究区面积的19.79%,覆盖了44%的生态空间、12.4%的海岸线、所有的重要物种栖息地及三分之一的古树名木。依照此生态保护红线研究进一步提出针对各类红线地块的保护和管理措施。研究提出的城市生态保护红线划定思路,可以为其他城市的重要生态空间保护、修复与管理提供参考。     

Climate Adaptation and Policy-Induced Inflation of Coastal Property Value

Human population density in the coastal zone and potential impacts of climate change underscore a growing conflict between coastal development and an encroaching shoreline. Rising sea-levels and increased storminess threaten to accelerate coastal erosion, while growing demand for coastal real estate encourages more spending to hold back the sea in spite of the shrinking federal budget for beach nourishment. As climatic drivers and federal policies for beach nourishment change, the evolution of coastline mitigation and property values is uncertain. We develop an empirically grounded, stochastic dynamic model coupling coastal property markets and shoreline evolution, including beach nourishment, and show that a large share of coastal property value reflects capitalized erosion control. The model is parameterized for coastal properties and physical forcing in North Carolina, U.S.A. and we conduct sensitivity analyses using property values spanning a wide range of sandy coastlines along the U.S. East Coast. The model shows that a sudden removal of federal nourishment subsidies, as has been proposed, could trigger a dramatic downward adjustment in coastal real estate, analogous to the bursting of a bubble. We find that the policy-induced inflation of property value grows with increased erosion from sea level rise or increased storminess, but the effect of background erosion is larger due to human behavioral feedbacks. Our results suggest that if nourishment is not a long-run strategy to manage eroding coastlines, a gradual removal is more likely to smooth the transition to more climate-resilient coastal communities.     

Beyond just sea‐level rise: considering macroclimatic drivers within coastal wetland vulnerability assessments to climate change

Due to their position at the land‐sea interface, coastal wetlands are vulnerable to many aspects of climate change. However, climate change vulnerability assessments for coastal wetlands generally focus solely on sea‐level rise without considering the effects of other facets of climate change. Across the globe and in all ecosystems, macroclimatic drivers (e.g., temperature and rainfall regimes) greatly influence ecosystem structure and function. Macroclimatic drivers have been the focus of climate change‐related threat evaluations for terrestrial ecosystems, but largely ignored for coastal wetlands. In some coastal wetlands, changing macroclimatic conditions are expected to result in foundation plant species replacement, which would affect the supply of certain ecosystem goods and services and could affect ecosystem resilience. As examples, we highlight several ecological transition zones where small changes in macroclimatic conditions would result in comparatively large changes in coastal wetland ecosystem structure and function. Our intent in this communication is not to minimize the importance of sea‐level rise. Rather, our overarching aim is to illustrate the need to also consider macroclimatic drivers within vulnerability assessments for coastal wetlands.     

Rapid risk assessment of wetland degradation and loss in low-lying coastal zone of Shanghai,China

Coastal wetlands are facing an increasingly high risk of degradation and loss due to a wide variety of human activities and natural processes. Human encroachment, including land reclamation, drainage, and introduction of invasive species, has direct negative effects on wetlands, mainly through changes in hydrology and vegetation. Additionally, accelerated sea level rise (SLR) can result in flooding of wetlands in low-lying coastal zones. In this study, we present a rapid risk assessment method for coastal wetland loss and degradation. The main stress factors, i.e., urban sprawl, agriculture, coastal erosion, and SLR, have been examined and quantified through remote sensing and geographic information system spatial analysis. A weighted factor-based linear model has been used to evaluate the spatial risk levels of wetland loss. The proposed methodology is applied to the low-lying coastal wetlands of Hangzhou Bay in Shanghai, China. The results show that the regions closer to the sea have relatively higher risk levels on the landward side of the coastline, but relatively low risk levels on the seaward side of the coastline. This work emphasizes the need to sustainably use and protect wetlands in order to reduce disaster risks and contribute to the improvement of human well-being.     

Learning from the past: Diatoms as palaeoecological indicators of changes in marine environments

The North Sea is seriously threatened by a variety of pollution sources. Terrestrially derived effluents are causing extensive environmental damage and changes to ecosystems of both the offshore and coastal waters. Coastal and estuarine communities are being lost to reclamation projects, and there is the future threat of rising sea level associaed with global warming. The spatial and temporal extent of recent anthropogenic changes are largely unknown due to the paucity of background information. The possible role of palaeoecological methodology in providing ‘reference levels’ against which current status can be compared, and their importance for restoration and policy decisions, are presented. The usefulness of diatoms as environmental indicators is illustrated. The extent of natural and anthropogenic changes on coastal habitats are demonstrated by reference to the Holocene evolution of the coastline of The Netherlands. Possible profitable areas for further research are outlined,e.g. a diatom nutrient calibration data set for shallow marine embayments.     

Predicted climate change,sea-level rise and wetland management in the Australian wet-dry tropics

The vulnerability of coastal areas in the Alligator Rivers Region (northern Australia) to predicted climate change and potential sea level rise was assessed as part of a national study. The coastal area is composed of a number of estuarine and freshwater habitats that are intricately interlinked and can not be effectively managed in isolation of each other. The outcomes of the assessment focused on the floodplain environments of the region, but are also applicable to the broader wetland environments that occur across the northern Australian wet-dry tropics. The management regime in the region is based on traditional Aboriginal ownership of much of the land, which is leased to the federal government as a national park. Scientific research has been intensive; however, important questions have been raised about the collation and effective use of this information. The vulnerability assessment framework required effective use of this information and cooperation with the management authority to identify change scenarios and management and research responses. A climate change scenario was established as the basis for predicting biophysical change in the coastal and wetland environments. The predictions suggest that large-scale change will occur and many of the existing values derived from these areas (i.e., usage by traditional Aboriginal occupants, and nature conservation) could be degraded or even lost. Recommended management responses include the initiation of specific monitoring, empowerment of local bodies to take active management steps, and to increase awareness of the likely consequences of change. Further data coordination and review are needed to ascertain the validity of the predictions and the concomitant management responses.     

全球变化主要过程对海滨生态系统生物入侵的影响

作为海陆交错带的海滨生态系统是海洋与陆地的过渡带, 是承受全球变化及其引起海平面上升等影响最为前沿、最为重要的缓冲带, 同时又是人类活动极为频繁和强烈的地带, 因此海滨生态系统是生物入侵的高发区之一。本文在分析海滨生态系统生物入侵现状的基础上, 分析了CO₂升高、海平面上升和富营养化等全球变化过程对海滨生态系统生物入侵的影响: CO₂浓度上升改变了入侵种的竞争态势, 海平面上升调整了入侵种的空间分布格局, 而富营养化为外来入侵种的进一步拓展提供了动力。为了深入揭示全球变化对海滨生态系统生物入侵过程的潜在影响, 很有必要在阐明单因子作用机制与过程的基础上加强与其他组分的交互作用研究, 以及中、长时间尺度上的动态分析。与此同时, 生物入侵导致的海滨生态系统变化对全球变化相关过程的反馈作用研究也具有极其重要的意义。     

Human-induced salinity changes impact marine organisms and ecosystems

Climate change is fundamentally altering marine and coastal ecosystems on a global scale. While the effects of ocean warming and acidification on ecology and ecosystem functions and services are being comprehensively researched, less attention is directed toward understanding the impacts of human-driven ocean salinity changes. The global water cycle operates through water fluxes expressed as precipitation, evaporation, and freshwater runoff from land. Changes to these in turn modulate ocean salinity and shape the marine and coastal environment by affecting ocean currents, stratification, oxygen saturation, and sea level rise. Besides the direct impact on ocean physical processes, salinity changes impact ocean biological functions with the ecophysiological consequences are being poorly understood. This is surprising as salinity changes may impact diversity, ecosystem and habitat structure loss, and community shifts including trophic cascades. Climate model future projections (of end of the century salinity changes) indicate magnitudes that lead to modification of open ocean plankton community structure and habitat suitability of coral reef communities. Such salinity changes are also capable of affecting the diversity and metabolic capacity of coastal microorganisms and impairing the photosynthetic capacity of (coastal and open ocean) phytoplankton, macroalgae, and seagrass, with downstream ramifications on global biogeochemical cycling. The scarcity of comprehensive salinity data in dynamic coastal regions warrants additional attention. Such datasets are crucial to quantify salinity-based ecosystem function relationships and project such changes that ultimately link into carbon sequestration and freshwater as well as food availability to human populations around the globe. It is critical to integrate vigorous high-quality salinity data with interacting key environmental parameters (e.g., temperature, nutrients, oxygen) for a comprehensive understanding of anthropogenically induced marine changes and its impact on human health and the global economy.     

基于土地利用/覆盖变化的中国大陆沿海地区生态状况评价

研究沿海地区土地利用变化及其对生态状况的影响,对于了解区域生态状况演变乃至全球变化具有重要意义.本研究以中国大陆沿海地区1980、1990、1995、2000、2005、2010和2015年7期土地利用/覆盖、高程及基础地理信息数据为关键数据源,利用生态等级指数法,对10个省级行政单位56个城市的生态状况进行综合评价,分析其时间动态演变和空间分异特征,深入探讨了高程分异及海陆梯度对我国大陆沿海地区生态状况的影响.结果表明:1980—2015年间,我国大陆沿海地区生态状况基本稳定,呈现逐步恶化、局部改善的特征.我国大陆沿海地区生态状况大致以杭州湾为界,呈南高北低的空间分异特征.大陆沿海地区生态等级指数高程分异显著,海拔<10 m的地区生态状况相对较差,海拔<30 m的区域在研究时段内生态状况的恶化趋势最为明显;研究区生态状况随着海拔的升高而增加,且海拔>400 m区域的生态状况在研究时段内呈现逐步好转的趋势.大陆沿海地区生态等级指数在海陆方向上亦存在梯度特征,自陆向海呈现高-低-高模式,距海10 km处生态状况变化最为显著,且随着距海距离的增加而降低.     

Human activities and climate variability drive fast‐paced change across the world's estuarine–coastal ecosystems

Time series of environmental measurements are essential for detecting, measuring and understanding changes in the Earth system and its biological communities. Observational series have accumulated over the past 2–5 decades from measurements across the world's estuaries, bays, lagoons, inland seas and shelf waters influenced by runoff. We synthesize information contained in these time series to develop a global view of changes occurring in marine systems influenced by connectivity to land. Our review is organized around four themes: (i) human activities as drivers of change; (ii) variability of the climate system as a driver of change; (iii) successes, disappointments and challenges of managing change at the sea‐land interface; and (iv) discoveries made from observations over time. Multidecadal time series reveal that many of the world's estuarine–coastal ecosystems are in a continuing state of change, and the pace of change is faster than we could have imagined a decade ago. Some have been transformed into novel ecosystems with habitats, biogeochemistry and biological communities outside the natural range of variability. Change takes many forms including linear and nonlinear trends, abrupt state changes and oscillations. The challenge of managing change is daunting in the coastal zone where diverse human pressures are concentrated and intersect with different responses to climate variability over land and over ocean basins. The pace of change in estuarine–coastal ecosystems will likely accelerate as the human population and economies continue to grow and as global climate change accelerates. Wise stewardship of the resources upon which we depend is critically dependent upon a continuing flow of information from observations to measure, understand and anticipate future changes along the world's coastlines.     

中国滨海盐沼湿地碳收支与碳循环过程研究进展

滨海盐沼湿地由于其较高的初级生产力和较缓慢的有机质降解速率而成为缓解全球变暖的有效蓝色碳汇,近年来引起全球范围内的热切关注.我国滨海盐沼湿地分布较广,国内学者对滨海盐沼湿地碳循环及碳收支研究取得了一定进展,深入研究滨海盐沼湿地碳循环有助于对全球碳循环及全球变化的理解,并为利用滨海湿地进行碳的增汇减排提供科学依据.主要从我国滨海盐沼湿地碳循环主要观测方法、碳收支与碳循环过程及特点、碳库的组成与影响因素、气态碳的输入输出、潮汐作用对其碳收支的影响这5个方面出发,对国内的滨海盐沼湿地碳循环与碳收支的研究进展进行了归纳总结,并对今后的研究方向给出如下建议:(1)加强滨海盐沼湿地土壤碳库在深度上和广度上的研究;(2)标准化滨海盐沼湿地碳储量、碳通量的量化方法和观测技术;(3)在研究尺度上要宏观、微观并重,同时加强长期原位监测湿地碳通量的变化与室内模拟研究;(4)量化在潮汐影响下滨海盐沼湿地碳与邻近生态系统之间的横向交换通量.只有对我国滨海盐沼湿地碳库收支进行更准确的评估和长期的碳库动态变化监测,方可进一步认识我国盐沼湿地对全球气候变化的影响及其反馈作用,这对于预测全球变化及制定湿地碳储备功能的提升策略具有重要的意义.