Short-term evolution pattern in salt marsh landscapes: the importance of physical constraints

IF 4 2区 环境科学与生态学 Q1 ECOLOGY Landscape Ecology Pub Date : 2024-05-03 DOI:10.1007/s10980-024-01898-w
Liming Xue, Tianyou Li, Xiuzhen Li, Yuxin Bi, Lin Su, Yuanhao Song, Wenzhen Zhao, Jianzhong Ge, Qing He, Benwei Shi
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Abstract

Context

Salt marsh landscapes at the land-sea interfaces exhibit contrasting spatiotemporal dynamics, resulting from varying physical constraints that limit new marsh establishment. The expansion of salt marsh landscapes towards the sea or their retreat towards the land is determined by patch-level changes, relying on the balance of power between the intrinsic biota traits and external physical disturbances.

Objectives

Examine how marsh dynamics respond to physical constraints, and clarify the pathway from coupled physical processes involving hydrodynamic forces, sediment transport, and morphological changes to rapid patch evolution and landscape changes.

Methods

We defined and distinguished four types of marsh changes based on patch proximities from five-month drone images in two typical marsh pioneer zones of the Yangtze Estuary, China: outlying expansion, edge expansion, infilling expansion, and retreat. Hydrodynamics and sediment transport were synchronously measured and compared near the two marsh edges, and morphological changes were generated by drone-derived digital elevation models (DEMs).

Results

We identified distinct seasonal patterns of net marsh expansion at the accretion-prone site, that is: Net marsh expansion started from the outlying expansion in spring, followed by edge expansion in summer and infilling expansion in autumn. However, at the erosion-prone site that experienced high bed shear stress, low sediment availability and high seaward sediment transport, we only observed limited infilling and edge expansion in spring. This suggests that the potential for long-distance patch formation beyond the initial marsh edges is diminished in areas subjected to intensive physical disturbances.

Conclusions

Patch evolution dynamics in response to site-specific physical constraints drive state differentiation of salt marsh landscape changes. Consequently, the heterogeneous evolution in salt marsh landscapes should be taken into account in restoration practice.

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盐沼地貌的短期演化模式:物理约束的重要性
背景海陆交界处的盐沼地貌呈现出截然不同的时空动态,这是由于限制新沼泽建立的物理约束条件不同造成的。盐沼景观向海洋扩展或向陆地退缩是由斑块级变化决定的,取决于内在生物群落特征与外部物理干扰之间的力量平衡。方法我们在中国长江口的两个典型沼泽先行区,根据为期五个月的无人机图像中的斑块邻近度,定义并区分了四种类型的沼泽变化:外围扩展、边缘扩展、填充扩展和退缩。对两个沼泽边缘附近的水动力和沉积物运移进行了同步测量和比较,并通过无人机获得的数字高程模型(DEM)生成了形态变化:沼泽净扩展始于春季的外围扩展,随后是夏季的边缘扩展和秋季的填充扩展。然而,在海床剪应力大、沉积物可用性低和向海沉积物迁移量大的易受侵蚀地点,我们只观察到春季有限的内填和边缘扩展。这表明,在受到强烈物理干扰的地区,最初沼泽边缘以外的长距离斑块形成的潜力减弱了。因此,在恢复实践中应考虑到盐沼景观的异质性演变。
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来源期刊
Landscape Ecology
Landscape Ecology 环境科学-地球科学综合
CiteScore
8.30
自引率
7.70%
发文量
164
审稿时长
8-16 weeks
期刊介绍: Landscape Ecology is the flagship journal of a well-established and rapidly developing interdisciplinary science that focuses explicitly on the ecological understanding of spatial heterogeneity. Landscape Ecology draws together expertise from both biophysical and socioeconomic sciences to explore basic and applied research questions concerning the ecology, conservation, management, design/planning, and sustainability of landscapes as coupled human-environment systems. Landscape ecology studies are characterized by spatially explicit methods in which spatial attributes and arrangements of landscape elements are directly analyzed and related to ecological processes.
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