北方湿地生态系统的木质侵蚀导致生长季节提前和延长

Hongchao Sun, Wen J. Wang, Zhihua Liu, Lei Wang, Suri G. Bao, Shengjie Ba, Yu Cong
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摘要

木本植物侵占(WPE)是全球普遍存在的一种生态现象,对生态系统结构和功能有重大影响。然而,人们对 WPE 如何影响中高纬度地区湿地生态系统的物候知之甚少。在此,我们利用 2001-2016 年期间的遥感数据集,研究了 WPE 对北方湿地生态系统生长季的开始(SOS)、高峰(POS)、结束(EOS)和长度(GSL)的区域尺度影响及其内在机制。我们的研究结果表明,WPE 使北方湿地的年 SOS 和 POS 提前,同时推迟了 EOS,延长了 GSL,这些影响随着时间的推移而增加。当北方湿地生态系统完全被木本植物侵占时,SOS 和 POS 分别提前了 12.17 天和 5.65 天,EOS 推迟了 2.74 天,GSL 延长了 15.21 天。我们还发现,WPE 对湿地 SOS 的影响主要归因于 WPE 程度(α)的增加,而气候因子在控制 POS 和 EOS 对 WPE 的响应方面发挥着更重要的作用。气候变化不仅直接影响湿地对 WPE 的物候反应,还通过调节土壤水分和 α 产生间接影响。WPE对SOS的影响主要由冬季降水和春季温度决定,对POS的影响主要由冬季降水、夏季温度和降水控制,对EOS的影响主要由冬季降水、夏季温度和秋季温度决定。我们的研究结果为理解 WPE 与湿地生态系统之间的相互作用提供了新的见解,强调了考虑 WPE 的影响对确保准确评估物候变化的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Woody encroachment induced earlier and extended growing season in boreal wetland ecosystems
Woody plant encroachment (WPE), a widespread ecological phenomenon globally, has significant impacts on ecosystem structure and functions. However, little is known about how WPE affects phenology in wetland ecosystems of middle and high latitudes. Here, we investigated the regional-scale effects of WPE on the start (SOS), peak (POS), end (EOS), and length (GSL) of the growing season in boreal wetland ecosystems, and their underlying mechanisms, using remote sensing dataset during 2001–2016. Our results showed that WPE advanced the annual SOS and POS, while delaying EOS and extending GSL in boreal wetlands with these impacts increasing over time. When boreal wetland ecosystems were fully encroached by woody plants, the SOS and POS were advanced by 12.17 and 5.65 days, respectively, the EOS was postponed by 2.74 days, and the GSL was extended by 15.21 days. We also found that the impacts of WPE on wetland SOS were predominantly attributed to the increased degree of WPE (α), while climatic factors played a more significant role in controlling the POS and EOS responses to WPE. Climate change not only directly influenced phenological responses of wetlands to WPE but also exerted indirect effects by regulating soil moisture and α. Winter precipitation and spring temperature primarily determined the effects of WPE on SOS, while its impacts on POS were mainly controlled by winter precipitation, summer temperature, and precipitation, and the effects on EOS were mainly determined by winter precipitation, summer temperature, and autumn temperature. Our findings offer new insights into the understanding of the interaction between WPE and wetland ecosystems, emphasizing the significance of considering WPE effects to ensure accurate assessments of phenology changes.
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