Soil carbon, nitrogen, and phosphorus storage in juniper–oak savanna: role of vegetation and geology

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2024-02-06 DOI:10.5194/soil-10-93-2024
Che-Jen Hsiao, Pedro A. M. Leite, Ayumi Hyodo, Thomas W. Boutton
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Abstract

Abstract. Woody-plant encroachment into grasslands and savannas has been globally widespread during the past century, likely driven by interactions between grazing, fire suppression, rising atmospheric CO2, and climate change. In the southernmost US Great Plains, Ashe juniper and live oak have increased in abundance. To evaluate potential interactions between this vegetation change and the underlying soil parent material on ecosystem biogeochemistry, we quantified soil organic carbon (SOC), total nitrogen (TN), total phosphorus (TP), and δ13C of SOC in soils obtained from trenches passing through grassland, juniper, and oak patches on soils lying atop the respective Edwards and Buda limestone formations in central Texas. Soils on the Edwards formation are more shallow and have more rock outcropping than those on Buda. The δ13C values of SOC under grasslands was −19 ‰, whereas those under woody patches were −21 ‰ to −24 ‰, indicating that wooded areas were relatively recent components of the landscape. Compared with grasslands, areas now dominated by juniper or oak had elevated SOC, TN, and TP storage in soils lying atop Edwards limestone. In Buda soils, only oak patches had increased SOC, TN, and TP storage compared with grasslands. Woody encroachment effects on soil nutrients were higher in soils on the Edwards formation, perhaps because root and litter inputs were more concentrated in the relatively shallow layer of soil atop the Edwards bedrock. Our findings suggest that geological factors should be considered when predicting nutrient store responses in savannas following vegetation change. Given that woody encroachment is occurring globally, our results have important implications for the management and conservation of these ecosystems. The potential interactive effects between vegetation change and soil parent material on C, N, and P storage warrant attention in future studies aimed at understanding and modeling the global consequences of woody encroachment.
杜松-橡树稀树草原的土壤碳、氮和磷储存:植被和地质的作用
摘要在过去的一个世纪中,木质植物对草地和稀树草原的侵占在全球范围内普遍存在,这可能是由放牧、火力压制、大气中二氧化碳含量上升和气候变化之间的相互作用所造成的。在美国大平原的最南端,杜松和栎树的数量有所增加。为了评估植被变化和下层土壤母质对生态系统生物地球化学的潜在相互作用,我们对位于得克萨斯州中部爱德华兹和布达石灰岩地层上的草地、杜松和栎树斑块土壤中的土壤有机碳(SOC)、总氮(TN)、总磷(TP)和 SOC 的 δ13C 进行了量化。爱德华兹岩层上的土壤比布达岩层上的土壤更浅,岩石露头也更多。草地下 SOC 的 δ13C 值为-19‰,而林木斑块下的 SOC δ13C 值为-21‰至-24‰,这表明林木区域是相对较新的地貌组成部分。与草地相比,现在以杜松或橡树为主的地区位于爱德华兹石灰岩上的土壤中的 SOC、TN 和 TP 储量较高。在布达土壤中,与草地相比,只有橡树斑块的 SOC、TN 和 TP 储量有所增加。在爱德华兹岩层上的土壤中,木质侵蚀对土壤养分的影响更大,这可能是因为根系和枯落物的输入更集中在爱德华兹基岩上相对较浅的土层中。我们的研究结果表明,在预测植被变化后热带稀树草原的养分储存反应时,应考虑地质因素。鉴于木质侵蚀正在全球范围内发生,我们的研究结果对这些生态系统的管理和保护具有重要意义。植被变化和土壤母质对碳、氮、磷贮存的潜在交互作用值得在今后的研究中加以关注,这些研究旨在了解和模拟林木侵蚀对全球造成的后果。
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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