Determining ecosystem functioning in Brazilian biomes through foliar carbon and nitrogen concentrations and stable isotope ratios
By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C...
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creator | Martinelli, L. A. Nardoto, G. B. Soltangheisi, A. Reis, C. R. G. Abdalla-Filho, A. L. Camargo, P. B. Domingues, T. F. Faria, D. Figueira, A. M. Gomes, T. F. Lins, S. R. M. Mardegan, S. F. Mariano, E. Miatto, R. C. Moraes, R. Moreira, M. Z. Oliveira, R. S. Ometto, J. P. H. B. Santos, F. L. S. Sena-Souza, J. Silva, D. M. L. Silva, J. C. S. S. Vieira, S. A. |
description | By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C) and nitrogen (N) concentrations, their isotope natural abundance and C:N ratio. In addition, we tested their correlations with mean annual temperature (MAT) and precipitation (MAP), as climatic factors. We found consistent differences in the C and N concentrations and their isotopic composition among the vegetation types. MAP is the main climatic driver of changes in N, C:N ratio, δ¹⁵N, and δ¹³C, correlating negatively with N and positively with C:N ratio. These relations show that these biomes follow an LES. The Caatinga had the highest δ¹⁵N values, suggesting that N residence time in soil is longer due to low leaching and plant uptake. We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. Finally, we expect our findings to contribute to a better understanding of the tropics in global climate models. |
doi_str_mv | 10.1007/s10533-020-00714-2 |
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A. ; Nardoto, G. B. ; Soltangheisi, A. ; Reis, C. R. G. ; Abdalla-Filho, A. L. ; Camargo, P. B. ; Domingues, T. F. ; Faria, D. ; Figueira, A. M. ; Gomes, T. F. ; Lins, S. R. M. ; Mardegan, S. F. ; Mariano, E. ; Miatto, R. C. ; Moraes, R. ; Moreira, M. Z. ; Oliveira, R. S. ; Ometto, J. P. H. B. ; Santos, F. L. S. ; Sena-Souza, J. ; Silva, D. M. L. ; Silva, J. C. S. S. ; Vieira, S. A.</creator><creatorcontrib>Martinelli, L. A. ; Nardoto, G. B. ; Soltangheisi, A. ; Reis, C. R. G. ; Abdalla-Filho, A. L. ; Camargo, P. B. ; Domingues, T. F. ; Faria, D. ; Figueira, A. M. ; Gomes, T. F. ; Lins, S. R. M. ; Mardegan, S. F. ; Mariano, E. ; Miatto, R. C. ; Moraes, R. ; Moreira, M. Z. ; Oliveira, R. S. ; Ometto, J. P. H. B. ; Santos, F. L. S. ; Sena-Souza, J. ; Silva, D. M. L. ; Silva, J. C. S. S. ; Vieira, S. A.</creatorcontrib><description>By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C) and nitrogen (N) concentrations, their isotope natural abundance and C:N ratio. In addition, we tested their correlations with mean annual temperature (MAT) and precipitation (MAP), as climatic factors. We found consistent differences in the C and N concentrations and their isotopic composition among the vegetation types. MAP is the main climatic driver of changes in N, C:N ratio, δ¹⁵N, and δ¹³C, correlating negatively with N and positively with C:N ratio. These relations show that these biomes follow an LES. The Caatinga had the highest δ¹⁵N values, suggesting that N residence time in soil is longer due to low leaching and plant uptake. We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. 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S.</creatorcontrib><creatorcontrib>Vieira, S. A.</creatorcontrib><title>Determining ecosystem functioning in Brazilian biomes through foliar carbon and nitrogen concentrations and stable isotope ratios</title><title>Biogeochemistry</title><addtitle>Biogeochemistry</addtitle><description>By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C) and nitrogen (N) concentrations, their isotope natural abundance and C:N ratio. In addition, we tested their correlations with mean annual temperature (MAT) and precipitation (MAP), as climatic factors. We found consistent differences in the C and N concentrations and their isotopic composition among the vegetation types. MAP is the main climatic driver of changes in N, C:N ratio, δ¹⁵N, and δ¹³C, correlating negatively with N and positively with C:N ratio. These relations show that these biomes follow an LES. The Caatinga had the highest δ¹⁵N values, suggesting that N residence time in soil is longer due to low leaching and plant uptake. We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. Finally, we expect our findings to contribute to a better understanding of the tropics in global climate models.</description><subject>Annual precipitation</subject><subject>Biogeochemistry</subject><subject>Biogeosciences</subject><subject>Carbon</subject><subject>Climate models</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecological function</subject><subject>Economics</subject><subject>Ecosystems</subject><subject>Environmental Chemistry</subject><subject>Global climate</subject><subject>Global climate models</subject><subject>Herbivores</subject><subject>Isotope ratios</subject><subject>Leaching</subject><subject>Leaves</subject><subject>Life Sciences</subject><subject>Nitrogen</subject><subject>ORIGINAL PAPERS</subject><subject>Plant cover</subject><subject>Residence time</subject><subject>Stable isotopes</subject><subject>Terrestrial ecosystems</subject><subject>Tropical environments</subject><subject>Uptake</subject><subject>Vegetation</subject><issn>0168-2563</issn><issn>1573-515X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kUtLAzEUhYMoWKt_QBACrkfzns5S6xMKbhTchSSTmaa0SU3SRd35z52H6M7V5d57zrnwXQDOMbrCCJXXCSNOaYEIKroWs4IcgAnmJS045u-HYIKwmBWEC3oMTlJaIYSqEtEJ-Lqz2caN88630JqQ9inbDWx23mQXhqnz8DaqT7d2ykPtwsYmmJcx7NolbEI3jdCoqIOHytfQuxxDaz00wRvrc1R9Thp2KSu9ttClkMPWwmGVTsFRo9bJnv3UKXh7uH-dPxWLl8fn-c2iMJThXBDKGbFGV7WhVKm65LOmEkIxoUtCNTOiZoJqpRirldWsEUTUuqwobUpeKUSn4HLM3cbwsbMpy1XYRd-dlISzHgiakU5FRpWJIaVoG7mNbqPiXmIke9RyRC071HJALXsTHU2pE_vWxr_of10Xo2uVcoi_d9isFKjqXvcNDoOOdQ</recordid><startdate>20210601</startdate><enddate>20210601</enddate><creator>Martinelli, L. 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A. ; Nardoto, G. B. ; Soltangheisi, A. ; Reis, C. R. G. ; Abdalla-Filho, A. L. ; Camargo, P. B. ; Domingues, T. F. ; Faria, D. ; Figueira, A. M. ; Gomes, T. F. ; Lins, S. R. M. ; Mardegan, S. F. ; Mariano, E. ; Miatto, R. C. ; Moraes, R. ; Moreira, M. Z. ; Oliveira, R. S. ; Ometto, J. P. H. B. ; Santos, F. L. S. ; Sena-Souza, J. ; Silva, D. M. L. ; Silva, J. C. S. S. ; Vieira, S. 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A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Determining ecosystem functioning in Brazilian biomes through foliar carbon and nitrogen concentrations and stable isotope ratios</atitle><jtitle>Biogeochemistry</jtitle><stitle>Biogeochemistry</stitle><date>2021-06-01</date><risdate>2021</risdate><volume>154</volume><issue>2</issue><spage>405</spage><epage>426</epage><pages>405-426</pages><issn>0168-2563</issn><eissn>1573-515X</eissn><abstract>By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C) and nitrogen (N) concentrations, their isotope natural abundance and C:N ratio. In addition, we tested their correlations with mean annual temperature (MAT) and precipitation (MAP), as climatic factors. We found consistent differences in the C and N concentrations and their isotopic composition among the vegetation types. MAP is the main climatic driver of changes in N, C:N ratio, δ¹⁵N, and δ¹³C, correlating negatively with N and positively with C:N ratio. These relations show that these biomes follow an LES. The Caatinga had the highest δ¹⁵N values, suggesting that N residence time in soil is longer due to low leaching and plant uptake. We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. Finally, we expect our findings to contribute to a better understanding of the tropics in global climate models.</abstract><cop>Cham</cop><pub>Springer Science + Business Media</pub><doi>10.1007/s10533-020-00714-2</doi><tpages>22</tpages><orcidid>https://orcid.org/0000-0002-7103-7551</orcidid></addata></record> |
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subjects | Annual precipitation Biogeochemistry Biogeosciences Carbon Climate models Earth and Environmental Science Earth Sciences Ecological function Economics Ecosystems Environmental Chemistry Global climate Global climate models Herbivores Isotope ratios Leaching Leaves Life Sciences Nitrogen ORIGINAL PAPERS Plant cover Residence time Stable isotopes Terrestrial ecosystems Tropical environments Uptake Vegetation |
title | Determining ecosystem functioning in Brazilian biomes through foliar carbon and nitrogen concentrations and stable isotope ratios |
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