A role for dendroecology in guiding hydrologic restoration and mitigating risks of peatland soil loss: an example from Chamaecyparis thyoides forests

IF 2.1 3区 农林科学 Q2 FORESTRY
Trees Pub Date : 2025-06-06 DOI:10.1007/s00468-025-02633-x
Robert B. Atkinson, Abigail Weaver, Joshua A. Kincaid, Frederic C. Wurster, James M. B. Doyle
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引用次数: 0

Key message

Tree rings of Chamaecyparis thyoides exhibit growth responses that are influenced by local hydrologic conditions through decadal timescales. That perspective can assist peatland natural resource managers in selection of hydrologic restoration targets that minimize chronic microbial oxidation and acute peat loss associated with fire.

Abstract

Temperate forested peatlands are valued for myriad ecosystem services including carbon storage and biodiversity which may be lost through anthropogenic disturbance of hydrologic regimes. Hydrologic alterations may be recorded in tree stem growth patterns and provide insights for management and restoration. In Chamaecyparis thyoides (Atlantic White Cedar, Juniper) swamps, stand drainage causes a shift from net soil carbon sink to source as microbial oxidation and catastrophic fire oxidize stored organic matter. Here, we analyze historic radial growth patterns in C. thyoides in order to characterize drainage history to guide hydrologic management for peat conservation and restoration. Basal area increment (BAI) estimates across a ~ 60-year chronology (1939–2003) were analyzed by flexible beta cluster analysis of 185 trees from 13 C. thyoides stands in the Great Dismal Swamp National Wildlife Refuge in Virginia and North Carolina, USA. Stands formed 3 groups, and growth rates among all groups were indicative of a drained hydrologic regime throughout the chronology compared to an undrained control stand. Regime shift analyses identified positive shifts for 2 stand groups in 1954 and for all 3 stand groups in 1963. Multiple response permutation procedures and partial mantel tests both identified two predictive growth variables including (1) visual observations of fluctuation in the water table and (2) proximity to a primary ditch. Growth rate was suppressed when weirs were installed in the mid-1980s; however, growth rebounded within ~ 2 years. The chronology ends when stands were struck by a major hurricane in 2003 and fires in 2008 and 2011 liberated 1.38 Tg of peat carbon. We conclude that dendroecology can detect hydrologic changes through time and can reduce risks of microbial oxidation and catastrophic fire in forested peatlands.

Abstract Image

Abstract Image

Abstract Image

树木生态学在指导水文恢复和减轻泥炭地土壤流失风险中的作用——以黄杉林为例。
关键信息:黄杉年轮在年代际尺度上表现出受当地水文条件影响的生长响应。这一观点可以帮助泥炭地自然资源管理者选择水文恢复目标,最大限度地减少慢性微生物氧化和与火灾有关的急性泥炭损失。摘要:温带森林泥炭地具有多种生态系统服务功能,包括碳储存和生物多样性,这些功能可能因人为水文干扰而丧失。水文变化可以记录在树木的生长模式中,并为管理和恢复提供见解。在Chamaecyparis thyoides(大西洋白雪松,杜松)沼泽中,林分排水导致微生物氧化和灾难性火灾氧化储存的有机物质,导致土壤净碳汇向来源转变。本文分析了泥炭的历史径向生长模式,以描述泥炭的排水历史,为泥炭保护和恢复的水文管理提供指导。采用灵活聚类分析方法,对美国维吉尼亚州和北卡罗来纳州大沼泽国家野生动物保护区13个山毛榉林185棵树的基础面积增量(basedarea increment, BAI)进行了近60年(1939-2003)年表分析。林分分为3个组,与不排水对照林分相比,所有组间的生长速率表明整个年代史上的排水水文状况。政权转移分析表明,1954年2个林分群和1963年3个林分群的变化均为正。多重响应排列程序和部分地幔试验都确定了两个预测增长变量,包括(1)地下水位波动的目视观察和(2)靠近主沟。20世纪80年代中期安装堰后,增长率受到抑制;然而,增长在大约2年内反弹。2003年的一场大飓风袭击了森林,2008年和2011年的大火释放了1.38 Tg的泥炭碳。我们得出结论,树木生态学可以检测随时间变化的水文变化,并可以降低森林泥炭地微生物氧化和灾难性火灾的风险。
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来源期刊
Trees
Trees 农林科学-林学
CiteScore
4.50
自引率
4.30%
发文量
113
审稿时长
3.8 months
期刊介绍: Trees - Structure and Function publishes original articles on the physiology, biochemistry, functional anatomy, structure and ecology of trees and other woody plants. Also presented are articles concerned with pathology and technological problems, when they contribute to the basic understanding of structure and function of trees. In addition to original articles and short communications, the journal publishes reviews on selected topics concerning the structure and function of trees.
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