Nitrogen availability and summer drought, but not N:P imbalance, drive carbon use efficiency of a Mediterranean tree-grass ecosystem

IF 10.8 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Richard Nair, Yunpeng Luo, Tarek El-Madany, Victor Rolo, Javier Pacheco-Labrador, Silvia Caldararu, Kendalynn A. Morris, Marion Schrumpf, Arnaud Carrara, Gerardo Moreno, Markus Reichstein, Mirco Migliavacca
{"title":"Nitrogen availability and summer drought, but not N:P imbalance, drive carbon use efficiency of a Mediterranean tree-grass ecosystem","authors":"Richard Nair,&nbsp;Yunpeng Luo,&nbsp;Tarek El-Madany,&nbsp;Victor Rolo,&nbsp;Javier Pacheco-Labrador,&nbsp;Silvia Caldararu,&nbsp;Kendalynn A. Morris,&nbsp;Marion Schrumpf,&nbsp;Arnaud Carrara,&nbsp;Gerardo Moreno,&nbsp;Markus Reichstein,&nbsp;Mirco Migliavacca","doi":"10.1111/gcb.17486","DOIUrl":null,"url":null,"abstract":"<p>All ecosystems contain both sources and sinks for atmospheric carbon (C). A change in their balance of net and gross ecosystem carbon uptake, ecosystem-scale carbon use efficiency (CUE<sub>ECO</sub>), is a change in their ability to buffer climate change. However, anthropogenic nitrogen (N) deposition is increasing N availability, potentially shifting terrestrial ecosystem stoichiometry towards phosphorus (P) limitation. Depending on how gross primary production (GPP, plants alone) and ecosystem respiration (R<sub>ECO</sub>, plants and heterotrophs) are limited by N, P or associated changes in other biogeochemical cycles, CUE<sub>ECO</sub> may change. Seasonally, CUE<sub>ECO</sub> also varies as the multiple processes that control GPP and respiration and their limitations shift in time. We worked in a Mediterranean tree-grass ecosystem (locally called ‘dehesa’) characterized by mild, wet winters and summer droughts. We examined CUE<sub>ECO</sub> from eddy covariance fluxes over 6 years under control, +N and + NP fertilized treatments on three timescales: annual, seasonal (determined by vegetation phenological phases) and 14-day aggregations. Finer aggregation allowed consideration of responses to specific patterns in vegetation activity and meteorological conditions. We predicted that CUE<sub>ECO</sub> should be increased by wetter conditions, and successively by N and NP fertilization. Milder and wetter years with proportionally longer growing seasons increased CUE<sub>ECO</sub>, as did N fertilization, regardless of whether P was added. Using a generalized additive model, whole ecosystem phenological status and water deficit indicators, which both varied with treatment, were the main determinants of 14-day differences in CUE<sub>ECO</sub>. The direction of water effects depended on the timescale considered and occurred alongside treatment-dependent water depletion. Overall, future regional trends of longer dry summers may push these systems towards lower CUE<sub>ECO</sub>.</p>","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":null,"pages":null},"PeriodicalIF":10.8000,"publicationDate":"2024-08-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/gcb.17486","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global Change Biology","FirstCategoryId":"93","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/gcb.17486","RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"BIODIVERSITY CONSERVATION","Score":null,"Total":0}
引用次数: 0

Abstract

All ecosystems contain both sources and sinks for atmospheric carbon (C). A change in their balance of net and gross ecosystem carbon uptake, ecosystem-scale carbon use efficiency (CUEECO), is a change in their ability to buffer climate change. However, anthropogenic nitrogen (N) deposition is increasing N availability, potentially shifting terrestrial ecosystem stoichiometry towards phosphorus (P) limitation. Depending on how gross primary production (GPP, plants alone) and ecosystem respiration (RECO, plants and heterotrophs) are limited by N, P or associated changes in other biogeochemical cycles, CUEECO may change. Seasonally, CUEECO also varies as the multiple processes that control GPP and respiration and their limitations shift in time. We worked in a Mediterranean tree-grass ecosystem (locally called ‘dehesa’) characterized by mild, wet winters and summer droughts. We examined CUEECO from eddy covariance fluxes over 6 years under control, +N and + NP fertilized treatments on three timescales: annual, seasonal (determined by vegetation phenological phases) and 14-day aggregations. Finer aggregation allowed consideration of responses to specific patterns in vegetation activity and meteorological conditions. We predicted that CUEECO should be increased by wetter conditions, and successively by N and NP fertilization. Milder and wetter years with proportionally longer growing seasons increased CUEECO, as did N fertilization, regardless of whether P was added. Using a generalized additive model, whole ecosystem phenological status and water deficit indicators, which both varied with treatment, were the main determinants of 14-day differences in CUEECO. The direction of water effects depended on the timescale considered and occurred alongside treatment-dependent water depletion. Overall, future regional trends of longer dry summers may push these systems towards lower CUEECO.

Abstract Image

氮供应量和夏季干旱(而非氮磷失衡)驱动地中海树草生态系统的碳利用效率
所有生态系统都包含大气碳(C)的源和汇。生态系统净碳吸收量和总碳吸收量平衡的变化,即生态系统尺度碳利用效率(CUEECO)的变化,是其缓冲气候变化能力的变化。然而,人为的氮(N)沉积正在增加氮的可用性,可能使陆地生态系统的化学计量转向磷(P)限制。根据氮、磷或其他生物地球化学循环的相关变化对初级生产总量(GPP,仅植物)和生态系统呼吸作用(RECO,植物和异养生物)的限制程度,CUEECO 可能会发生变化。从季节上看,CUEECO 也会随着控制 GPP 和呼吸作用的多个过程及其限制因素的变化而变化。我们在一个地中海树草生态系统(当地称为 "dehesa")中工作,该生态系统的特点是冬季温和湿润,夏季干旱。我们从涡度协方差通量中考察了 6 年来在对照、+N 和 +NP 施肥处理下的 CUEECO,考察了三种时间尺度:年度、季节(由植被物候期决定)和 14 天聚合。更精细的聚合可考虑对植被活动和气象条件特定模式的响应。我们预测,CUEECO 应在较潮湿的条件下增加,并在氮和磷肥的作用下相继增加。较温和、较湿润的年份,生长季节相应较长,CUEECO 会增加,施氮肥也会增加,无论是否添加磷肥。利用广义加法模型,整个生态系统的物候状态和缺水指标是决定 14 天 CUEECO 差异的主要因素。水分效应的方向取决于所考虑的时间尺度,并且与处理相关的水分耗竭同时发生。总体而言,未来干旱夏季延长的区域趋势可能会使这些系统的 CUEECO 值降低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信