{"title":"氮添加和气候变暖对地上和地下氮保留的短期和长期影响","authors":"Benjamin F. A. Souriol, Hugh A. L. Henry","doi":"10.1007/s11104-024-06889-z","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Background and aims</h3><p>Increased atmospheric nitrogen (N) deposition and climate warming can both exert strong, cumulative effects on N losses from ecosystems. However, given their potential interactions with interannual variability in environmental conditions or other factors, it is uncertain how effectively the comparison of short- vs. long-term results from N addition and warming field experiments can reveal these cumulative effects. Our aim was to compare the short-term versus long-term effects of N addition and warming on aboveground and belowground N retention while controlling for interannual variation in other factors.</p><h3 data-test=\"abstract-sub-heading\">Methods</h3><p>We added <sup>15</sup>N tracer to N addition and warming plots in a northern temperate grass-dominated old field in early spring, then assessed the amount of the added <sup>15</sup>N recovered aboveground and belowground at the peak of the growing season. We controlled for interannual variation in background environmental conditions by comparing new N addition and warming plots (3 years old) to those of an existing field experiment (16 years old).</p><h3 data-test=\"abstract-sub-heading\">Results</h3><p>Both N addition and warming significantly increased aboveground and belowground <sup>15</sup>N tracer retention. However, there were no significant interactions between either of the treatments and plot age for <sup>15</sup>N tracer retention, nor for plant production. The lack of interactions with plot age corresponded with the continued dominance of two non-native grass species in the plots.</p><h3 data-test=\"abstract-sub-heading\">Conclusion</h3><p>Our results highlight the potentially important role of dominant species that resist replacement in buffering against the effects of global change on cumulative, long-term changes in ecosystem N retention.</p>","PeriodicalId":20223,"journal":{"name":"Plant and Soil","volume":null,"pages":null},"PeriodicalIF":3.9000,"publicationDate":"2024-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Short- versus long-term effects of nitrogen addition and warming on aboveground and belowground nitrogen retention\",\"authors\":\"Benjamin F. A. Souriol, Hugh A. L. Henry\",\"doi\":\"10.1007/s11104-024-06889-z\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<h3 data-test=\\\"abstract-sub-heading\\\">Background and aims</h3><p>Increased atmospheric nitrogen (N) deposition and climate warming can both exert strong, cumulative effects on N losses from ecosystems. However, given their potential interactions with interannual variability in environmental conditions or other factors, it is uncertain how effectively the comparison of short- vs. long-term results from N addition and warming field experiments can reveal these cumulative effects. Our aim was to compare the short-term versus long-term effects of N addition and warming on aboveground and belowground N retention while controlling for interannual variation in other factors.</p><h3 data-test=\\\"abstract-sub-heading\\\">Methods</h3><p>We added <sup>15</sup>N tracer to N addition and warming plots in a northern temperate grass-dominated old field in early spring, then assessed the amount of the added <sup>15</sup>N recovered aboveground and belowground at the peak of the growing season. We controlled for interannual variation in background environmental conditions by comparing new N addition and warming plots (3 years old) to those of an existing field experiment (16 years old).</p><h3 data-test=\\\"abstract-sub-heading\\\">Results</h3><p>Both N addition and warming significantly increased aboveground and belowground <sup>15</sup>N tracer retention. However, there were no significant interactions between either of the treatments and plot age for <sup>15</sup>N tracer retention, nor for plant production. The lack of interactions with plot age corresponded with the continued dominance of two non-native grass species in the plots.</p><h3 data-test=\\\"abstract-sub-heading\\\">Conclusion</h3><p>Our results highlight the potentially important role of dominant species that resist replacement in buffering against the effects of global change on cumulative, long-term changes in ecosystem N retention.</p>\",\"PeriodicalId\":20223,\"journal\":{\"name\":\"Plant and Soil\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2024-08-13\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Plant and Soil\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://doi.org/10.1007/s11104-024-06889-z\",\"RegionNum\":2,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"AGRONOMY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Plant and Soil","FirstCategoryId":"97","ListUrlMain":"https://doi.org/10.1007/s11104-024-06889-z","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"AGRONOMY","Score":null,"Total":0}
Short- versus long-term effects of nitrogen addition and warming on aboveground and belowground nitrogen retention
Background and aims
Increased atmospheric nitrogen (N) deposition and climate warming can both exert strong, cumulative effects on N losses from ecosystems. However, given their potential interactions with interannual variability in environmental conditions or other factors, it is uncertain how effectively the comparison of short- vs. long-term results from N addition and warming field experiments can reveal these cumulative effects. Our aim was to compare the short-term versus long-term effects of N addition and warming on aboveground and belowground N retention while controlling for interannual variation in other factors.
Methods
We added 15N tracer to N addition and warming plots in a northern temperate grass-dominated old field in early spring, then assessed the amount of the added 15N recovered aboveground and belowground at the peak of the growing season. We controlled for interannual variation in background environmental conditions by comparing new N addition and warming plots (3 years old) to those of an existing field experiment (16 years old).
Results
Both N addition and warming significantly increased aboveground and belowground 15N tracer retention. However, there were no significant interactions between either of the treatments and plot age for 15N tracer retention, nor for plant production. The lack of interactions with plot age corresponded with the continued dominance of two non-native grass species in the plots.
Conclusion
Our results highlight the potentially important role of dominant species that resist replacement in buffering against the effects of global change on cumulative, long-term changes in ecosystem N retention.
期刊介绍:
Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.