Dendrochronologia最新文献

{"title":"Growth rates and responses to climate and aridity of Algerian Atlas pistachio populations","authors":"Naima Ifticene-Habani ,&nbsp;J. Julio Camarero ,&nbsp;Fatiha Abdoun","doi":"10.1016/j.dendro.2025.126326","DOIUrl":"10.1016/j.dendro.2025.126326","url":null,"abstract":"<div><div>The Atlas pistachio (<em>Pistacia atlantica</em>) is a minor hardwood species threatened due to overexploitation in some regions of the Maghreb, but it shows an extraordinary ecological plasticity inhabiting sites subjected from Mediterranean humid to arid conditions. To assess the drought tolerance of this understudied species, we sampled three Algerian populations along a N-S gradient of increasing aridity: Theniet el Had (sub-humid site, H), Djelba (semi-arid or dry site, D) and Béchar (arid site, A). First, ring-width chronologies were built. Second, correlations between ring-width indices, climate variables, a drought index and teleconnection indices (NAO, North Atlantic Oscillation; MOI, Mediterranean Oscillation index; SOI, Southern Oscillation Index; SaOI, Sahara Oscillation Index) were calculated. A high precipitation in the previous autumn and winter enhanced radial growth of Atlas pistachio and also high June precipitation in the wettest site H. In the driest site A, high maximum temperatures in spring constrained growth. High minimum temperatures in late summer and early autumn enhanced growth in sites D and A, which showed similar year-to-year growth variability (<em>r</em> = 0.426, <em>p</em> = 0.015, period 1980–2011). Correlations with a drought index peaked in the driest site A from September to December. Positive relationships between growth and drought indices in spring and autumn suggest a bimodal growth pattern. The three sites showed positive correlations between growth indices and the April MOI. However, negative relationships were found for January NAO or MOI and spring indices (June NAO, May SOI) in site H. Here, growth rates were negatively related to the SaOI. The Atlas pistachio shows a remarkable drought tolerance and its climate-growth relationships indicate plastic growth responses to precipitation variability.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126326"},"PeriodicalIF":2.7,"publicationDate":"2025-03-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143642860","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Corrigendum to “Pointer years revisited: Does one method fit all? A clarifying discussion” [Dendrochronologia 78 (2023) 126064]","authors":"Gottfried Jetschke ,&nbsp;Ernst van der Maaten ,&nbsp;Marieke van der Maaten-Theunissen","doi":"10.1016/j.dendro.2025.126323","DOIUrl":"10.1016/j.dendro.2025.126323","url":null,"abstract":"","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126323"},"PeriodicalIF":2.7,"publicationDate":"2025-03-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143611183","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Picea abies and Pinus cembra at high altitudes show different growth reaction to rising temperatures: Study from the Western Carpathian subalpine forests","authors":"Peter Marcis ,&nbsp;Jergus Rybar ,&nbsp;Vladimír Šebeň ,&nbsp;Vlastimil Murgaš ,&nbsp;Zuzana Sitková","doi":"10.1016/j.dendro.2025.126325","DOIUrl":"10.1016/j.dendro.2025.126325","url":null,"abstract":"<div><div>The subalpine forests of the Western Carpathian High Tatra Mountains represent a unique, isolated enclave of postglacial refugia. Climate change presents challenges and opportunities for alpine species: while rising temperatures may extend the growing season, potentially boosting growth rates, these changes may also push species closer to their physiological limits. This study examines the impacts of warming on the radial growth of <em>Picea abies</em> Karst. and <em>Pinus cembra</em> L. in Western Carpathian subalpine forests. We hypothesize that in subalpine zones, where tree growth is predominantly limited by low temperatures, <em>Picea abies</em> will experience enhanced growth under warmer conditions, whereas <em>Pinus cembra</em> will reduce growth under associated stress. We identified two pointer years with negative growth responses in <em>P. cembra</em> (1980 and 2014) and two years (1974 and 1993) with negative growth responses observed only in <em>P. abies</em>. The years 1965 and 1996 were found to be common years of negative response. Results indicate a non-linear relationship between temperature and radial increment. While <em>P. abies</em> and <em>P. cembra</em> both respond negatively to cold years (RWI &lt; 1) at lower temperature sums, their responses diverge at higher temperature sums. As the cumulative sum of daily average temperatures above 9°C exceeds 1500 degree-days, spruce’s response remains positive (RWI &gt; 1), whereas stone pine´s becomes significantly negative (RWI &lt; 0.9). We conclude that, with continued climate manifestations, such as heatwaves, the competitive advantage of spruce in subalpine forests could potentially result in a gradual contraction of <em>P. cembra</em> distribution in the High Tatra Mountains.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126325"},"PeriodicalIF":2.7,"publicationDate":"2025-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143642859","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Elevation-dependent breakpoint in climate forcing of tree growth in the Turtmann River Basin, Switzerland","authors":"Nazimul Islam ,&nbsp;Torsten Vennemann ,&nbsp;David Meko ,&nbsp;Stuart Lane","doi":"10.1016/j.dendro.2025.126322","DOIUrl":"10.1016/j.dendro.2025.126322","url":null,"abstract":"<div><div>Tree rings are valuable proxies for reconstructing changes in climate at annual and intra-annual resolutions. In Alpine regions, changes in climate may well lead to switches between tree-growth being temperature-limited and precipitation-limited. Distinguishing between these is important as they may express themselves differently in tree rings. However, such switches cannot be separated from more local environmental influences such as elevation and aspect. In this study, we seek to understand how tree growth evolves as a function of elevation in the context of climate change. For the growth of European larch (<em>Larix decidua</em> Mill) in the Turtmann River Basin, a glacier-fed high-elevation river basin in the Swiss Alps, located in southwestern Switzerland, we find that the average temperature increase leads to a switch from temperature-limitation to precipitation-limitation as a function of elevation. The growth of <em>Larix decidua</em> Mill in this river basin is influenced by previous year’s September-October-November (SON) temperature and current year’s January-February-March (JFM) precipitation in the higher- and lower-elevations across an elevational gradient respectively. Based on the analysis from four sites, assuming a linear response, our study suggests that there is a transition zone (i.e., an elevational breakpoint) between 1800 and 900 m AMSL where the signal changes from precipitation-limited to temperature-limited. We also conclude that this elevation breakpoint appears to be rising with time due to increasingly warmer annual average temperatures in this Alpine setting, where this warming is noted to be more than twice compared to the global average temperature change.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126322"},"PeriodicalIF":2.7,"publicationDate":"2025-03-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143637421","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The carbon-14 bomb peak as a turning point in dendrochronology in tropics: A literature review and case study with Araucaria angustifolia","authors":"Cláudia Fontana ,&nbsp;Milena Godoy-Veiga ,&nbsp;Lidio López ,&nbsp;Luiz Carlos Pessenda ,&nbsp;Bruna Hornink ,&nbsp;Gabriel Assis-Pereira ,&nbsp;Marcelo Callegari Scipioni ,&nbsp;Francisco William da Cruz ,&nbsp;Mario Tomazello-Filho ,&nbsp;Ricardo Villalba","doi":"10.1016/j.dendro.2025.126310","DOIUrl":"10.1016/j.dendro.2025.126310","url":null,"abstract":"<div><div>Establishing reliable tree-ring chronologies in the tropics remains a challenge, however, it can be mitigated by combining direct and indirect methods. This study investigates the synergy between classical dendrochronology and radiocarbon (¹⁴C) dating. For this purpose, we developed a preliminary chronology for <em>Araucaria angustifolia</em> in southern Brazil and a compilation of ¹⁴C applications in Brazilian dendrochronology. We tested the synchronicity of tree growth using classical dendrochronological methods on samples from three trees. Radiocarbon analysis of selected tree rings, specifically those formed during the ¹⁴C bomb peak, confirmed the annual nature of growth rings and validated the accuracy of our classical dating. While initial dating discrepancies were observed, these were resolved by considering the variability in the onset of cambial activity for this species. The mean series intercorrelation increased after analyzing the synchronicity in tree growth variability (number of samples n = 3, period 1930–2018) before (<em>r</em> = 0.366) and after (<em>r</em> = 0.423) the adjustments. Our findings demonstrate the effectiveness of combining classical dendrochronology and ¹⁴C dating to establish robust chronologies, particularly for tropical and subtropical species such as <em>A. angustifolia</em> that present dating challenges. This preliminary chronology provides a robust reference for developing a more comprehensive and well-replicated <em>A. angustifolia</em> chronology for subtropical Brazil. Additionally, the literature review showed that radiocarbon dating studies in Brazil, while still relatively scarce (21 studies) and with an uneven geographic distribution, have significantly advanced over the past 5 years. Our case study highlights the growing importance of ¹⁴C analysis in tree-ring research in Brazil and emphasizes the need for further studies to refine ¹⁴C calibration curves for the Southern Hemisphere.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126310"},"PeriodicalIF":2.7,"publicationDate":"2025-02-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143548918","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Tree-ring oxygen isotope cross-dating between southeastern China and central Japan","authors":"Shiyuan Shi ,&nbsp;Jiangfeng Shi ,&nbsp;Takeshi Nakatsuka ,&nbsp;Masaki Sano ,&nbsp;Zhen Li ,&nbsp;Jiaping Shu ,&nbsp;Xiaoying Wang ,&nbsp;Jianqiu Huang ,&nbsp;Jinbao Li ,&nbsp;Huayu Lu","doi":"10.1016/j.dendro.2025.126319","DOIUrl":"10.1016/j.dendro.2025.126319","url":null,"abstract":"<div><div>Long tree-ring chronologies applicable for archaeological dating are extremely rare in southeastern China, limiting dendroarchaeological research in this monsoon region. A large number of archaeological woods have been unearthed in this region, and the application of tree-ring oxygen isotope (δ¹⁸O) allows cross-dating of less climatically stressed trees of different species from distant sites, offering a potential to change the standstill. In this study, we tested tree-ring δ¹⁸O cross-dating of modern and archaeological samples from southeastern China against the central Japan master tree-ring chronology spanning the past 2872 years. Dating experiments on living-tree chronologies of known ages indicate that it is feasible to pinpoint their correct calendar dates using the central Japan master chronology. Cross-dating based on tree-ring width was successfully conducted on 46 <em>Cunninghamia lanceolata</em> samples excavated from Han Dynasty tombs in the Yangzhou area, southeastern China, and the sample with the most recent ring was selected to build a floating tree-ring δ¹⁸O series. The floating series was cross-dated with the central Japan master chronology to produce an unambiguous end date of 2 BCE, which is supported by climate records in historical literature. The success of δ¹⁸O dating is dependent on common signals at both high and low frequencies originating from multi-scale climate coherence between the two regions, and thus long sample series containing decadal to multidecadal variations are necessary. Our study shows a feasibility of δ¹⁸O-based dendroarchaeology in southeastern China.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126319"},"PeriodicalIF":2.7,"publicationDate":"2025-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143580107","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Blue intensity, tree-ring dimensions, earlywood vessels and flood rings in floodplain Fraxinus pennsylvanica trees, central Canada","authors":"Jacques C. Tardif ,&nbsp;Ryszard J. Kaczka ,&nbsp;France Conciatori","doi":"10.1016/j.dendro.2025.126311","DOIUrl":"10.1016/j.dendro.2025.126311","url":null,"abstract":"<div><div>Flood rings have been identified in numerous floodplain ring-porous tree species of the genus <em>Fraxinus</em> and <em>Quercus</em>. They are generally characterized by an earlywood having more numerous vessels with smaller cross-sectional area compared to “normal” tree ring. In recent years, blue intensity (BI) has developed as a surrogate method to determine tree-ring density. The method, so far, has been restricted to coniferous species. No studies have assessed the utility of BI in floodplain ring-porous species and its association, among others, with earlywood vessel features and hydrological conditions. In this study, twenty green ash (<em>Fraxinus pennsylvanica</em> Marsh.) trees were analysed. Flood rings were identified with both cross-sectional area of all earlywood vessels ≥ 1000 µm² and BI measured. Results indicated strong associations among given BI, tree-ring dimension, earlywood vessel and flood-ring chronologies. For instance, both earlywood BI (especially EW10BI) and Delta BI (DBI) showed significant inversed associations with earlywood porosity and with flood-ring abundance. These BI parameters were also strongly associated with spring discharge. In green ash, tree rings formed in years leading to flood-ring formation were characterized by increased earlywood density (higher blue intensity caused by an alteration in size and arrangement of earlywood vessels) and, to a lesser extent, by reduced latewood density. The BI features derived from the earlywood and the entire tree ring both prove to effectively complement visual identification of flood ring. Blue intensity in ring-porous species may prove useful in dendrohydrological reconstructions and also in wood sciences, i.e., when estimating tree-ring density is desired. In regards to ring-porous species, further work is warranted comparing software differences in determining BI, evaluating BI signal in other species and from various hydrological regimes.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126311"},"PeriodicalIF":2.7,"publicationDate":"2025-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143611182","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Should I stay or should I go? Meteorological effects on radial growth in introduced lodgepole pine provenances","authors":"Diāna Jansone ,&nbsp;Roberts Matisons ,&nbsp;Didzis Elferts ,&nbsp;Kalev Jõgiste ,&nbsp;Baiba Jansone ,&nbsp;Inga Straupe ,&nbsp;Āris Jansons","doi":"10.1016/j.dendro.2025.126308","DOIUrl":"10.1016/j.dendro.2025.126308","url":null,"abstract":"<div><div>Climate change poses significant challenges to tree survival and productivity, necessitating the introduction of non-native species to enhance forest resilience. This study examines the sensitivity of different lodgepole pine (<em>Pinus contorta</em>) provenances to meteorological conditions in Latvia compared to native Scots pine (<em>Pinus sylvestris</em>). The study was carried out in lodgepole pine provenance trials at two locations in Latvia. It analyzed 12 provenances of <em>Pinus contorta</em> from Canada, one <em>Pinus contorta</em> grown in Latvia, and one <em>Pinus sylvestris</em> grown in Latvia. The age of the experimental trials ranged from 29 to 38 years. Data analysis involved climate sensitivity analysis, including cluster analysis, correlation analysis and linear-mixed effects model, to examine the relationship between radial growth patterns and meteorological variables. Complex meteorological influences on TRW were revealed, identifying eight significant predictors primarily associated with spring and summer conditions. The most substantial effects were linked to climatic water balance in spring, winter temperatures, and summer precipitation. Site conditions significantly influenced growth more than genetic effect between provenances. The Lacobie Creek provenance, originating from the central part of the natural distribution area demonstrated lower sensitivity to climatic variables and was the most productive, indicating a lower risk from climate-related challenges and promising future growth potential. In general, the variation in weather sensitivity across provenances was similar. Testing under local site conditions is essential to evaluate the potential for introducing non-native provenances, as their performance compared to native species can vary depending on the specific environmental conditions.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126308"},"PeriodicalIF":2.7,"publicationDate":"2025-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143562153","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Long-term tree growth-climate relationships of Fagus orientalis Lipsky at high-elevation forest edges in the Alborz Mountains, northern Iran","authors":"Halime Moradi,&nbsp;Niels Schwab,&nbsp;Udo Schickhoff","doi":"10.1016/j.dendro.2025.126306","DOIUrl":"10.1016/j.dendro.2025.126306","url":null,"abstract":"<div><div>Rapid warming at high elevations may increase the sensitivity of tree growth to climatic signals. While several studies have examined tree growth in the Hyrcanian forests of the Alborz Mountains (Iran), the impact of climatic factors on <em>Fagus orientalis</em> Lipsky at its upper growth limit remains unclear. This study investigates the relationship between the annual tree-ring width of <em>Fagus orientalis</em> and climate over more than a century at its elevational growth limit. We constructed two tree-ring width chronologies from cores collected at elevations of 2400–2550 m a.s.l. at two contrasting sites in the Hyrcanian Forest, which differ in soil physical conditions. We correlated the tree-ring data with monthly mean temperature, precipitation sums, and the six-month standardized precipitation-evapotranspiration index. Our results show that moisture deficit, particularly during the growing season (June to November), is a critical factor affecting growth. Precipitation has a more pronounced influence on growth at high elevations compared to lower elevations in the Hyrcanian Forests, suggesting that <em>Fagus orientalis</em> is more dependent on precipitation and soil moisture during summer and autumn drought stress. The distance from the Caspian Sea and the constellation of local climatic factors such as low precipitation and high irradiation are likely to contribute to reduced moisture availability at higher elevations. Divergent results from contrasting sites highlight the important role of soil physical conditions in shaping growth-climate relationships. This study provides valuable insights into the radial growth-climate relationships of <em>Fagus orientalis</em> at elevated sites, and enhances our understanding of the sensitivity of the species in response to future climate change.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126306"},"PeriodicalIF":2.7,"publicationDate":"2025-02-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143511821","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Changing climate response of Northeast Ohio white oaks, USA: Is it tree age or site age?","authors":"Gregory Wiles,&nbsp;Nicholas Wiesenberg,&nbsp;Meagen Pollock,&nbsp;Caitlyn Denes,&nbsp;Tyrell Cooper,&nbsp;Desiree Smith,&nbsp;Melita Wiles","doi":"10.1016/j.dendro.2025.126307","DOIUrl":"10.1016/j.dendro.2025.126307","url":null,"abstract":"<div><div>White oak, a keystone species of the broadleaf forests of the North American Midwest, has a significant role in providing ecosystems services in a region experiencing warming and increasingly pluvial conditions. A one-hundred-year-old white oak stand in an arboretum, along with two second growth (∼200-year-old) stands from Northeast Ohio have consistently responded positively to summer (June-July) precipitation over the past century, whereas four nearby old growth sites (&gt;300 years old) have lost their moisture sensitivity since about the mid 1970s. This “fading drought signal,” which has been previously reported, appears to be more a result of the legacy of land use at the individual sites rather than tree age. The younger oak stands and their relative sustained drought sensitivity is also related to their history of recently attaining the canopy and similar responses associated with intervals of selective logging. All sites are strongly, negatively correlated with summer (June-July) maximum monthly temperatures and in general the maximum temperatures are negatively correlated with precipitation in those months. Future warming in the Midwest is projected to see increases in spring precipitation and likely decreases in late summer precipitation linked to a northward migration of the North American Westerly Jet. This projected decrease in summer precipitation coupled with an increase in maximum and minimum summer temperatures in the coming decades would increase the moisture stress on these trees. Our examination of these varying climate responses with respect to site characteristics and forest age can help future assessments of tree health and the forest’s ability to sequester carbon, as well as facilitate efforts to reconstruct climate by using a range of tree sites for intervals when sensitivity in old growth sites is lost.</div></div>","PeriodicalId":50595,"journal":{"name":"Dendrochronologia","volume":"91 ","pages":"Article 126307"},"PeriodicalIF":2.7,"publicationDate":"2025-02-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143535351","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}