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Damasceno AR, Garcia S, Aleixo IF, Menezes JCG, Pereira IS, De Kauwe MG, Ferrer VR, Fleischer K, Grams TEE, Guedes AV, Hartley IP, Kruijt B, Lugli LF, Martins NP, Norby RJ, Pires-Santos JS, Portela BTT, Rammig A, de Oliveira LR, Santana FD, Santos YR, de Souza CCS, Ushida G, Lapola DM, Quesada CAN, Domingues TF. In situ short-term responses of Amazonian understory plants to elevated CO 2. PLANT, CELL & ENVIRONMENT 2024; 47:1865-1876. [PMID: 38334166 DOI: 10.1111/pce.14842] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/23/2023] [Revised: 01/16/2024] [Accepted: 01/23/2024] [Indexed: 02/10/2024]
Abstract
The response of plants to increasing atmospheric CO2 depends on the ecological context where the plants are found. Several experiments with elevated CO2 (eCO2) have been done worldwide, but the Amazonian forest understory has been neglected. As the central Amazon is limited by light and phosphorus, understanding how understory responds to eCO2 is important for foreseeing how the forest will function in the future. In the understory of a natural forest in the Central Amazon, we installed four open-top chambers as control replicates and another four under eCO2 (+250 ppm above ambient levels). Under eCO2, we observed increases in carbon assimilation rate (67%), maximum electron transport rate (19%), quantum yield (56%), and water use efficiency (78%). We also detected an increase in leaf area (51%) and stem diameter increment (65%). Central Amazon understory responded positively to eCO2 by increasing their ability to capture and use light and the extra primary productivity was allocated to supporting more leaf and conducting tissues. The increment in leaf area while maintaining transpiration rates suggests that the understory will increase its contribution to evapotranspiration. Therefore, this forest might be less resistant in the future to extreme drought, as no reduction in transpiration rates were detected.
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Affiliation(s)
- Amanda Rayane Damasceno
- Ecology Graduate Program, National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Sabrina Garcia
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Izabela Fonseca Aleixo
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | | | - Iokanam Sales Pereira
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | | | - Vanessa Rodrigues Ferrer
- Ecology Graduate Program, National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | | | - Thorsten E E Grams
- School of Life Sciences, Technical University of Munich (TUM), Freising, Germany
| | - Alacimar V Guedes
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Iain Paul Hartley
- Geography, Faculty of Environment, Science and Economy, University of Exeter, Exeter, UK
| | - Bart Kruijt
- Wageningen University, Water Systems and Global Change, Wageningen, Netherlands
| | | | - Nathielly Pires Martins
- Tropical Forest Sciences Graduate Program, National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Richard J Norby
- School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, UK
| | | | - Bruno Takeshi Tanaka Portela
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Anja Rammig
- School of Life Sciences, Technical University of Munich (TUM), Freising, Germany
| | - Leonardo Ramos de Oliveira
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Flávia Delgado Santana
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Yago Rodrigues Santos
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | | | - Gabriela Ushida
- Ecology Graduate Program, National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - David Montenegro Lapola
- Laboratório de Ciência do Sistema Terrestre - LabTerra, Centro de Pesquisas Meteorológicas e Climáticas Aplicadas à Agricultura - CEPAGRI, Universidade Estadual de Campinas - UNICAMP, Campinas, São Paulo, Brazil
| | - Carlos Alberto Nobre Quesada
- Environmental Dynamics Coordination (CODAM), National Institute for Amazonian Research (INPA), Manaus, Amazonas, Brazil
| | - Tomas Ferreira Domingues
- Faculdde de Filosofia, Ciências e Letras de Ribeirão Preto, Departamento de Biologia, Universidade de São Paulo, Ribeirão Preto, São Paulo, Brazil
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Cordeiro AL, Norby RJ, Andersen KM, Valverde‐Barrantes O, Fuchslueger L, Oblitas E, Hartley IP, Iversen CM, Gonçalves NB, Takeshi B, Lapola DM, Quesada CA. Fine-root dynamics vary with soil depth and precipitation in a low-nutrient tropical forest in the Central Amazonia. PLANT-ENVIRONMENT INTERACTIONS (HOBOKEN, N.J.) 2020; 1:3-16. [PMID: 37284129 PMCID: PMC10168058 DOI: 10.1002/pei3.10010] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 10/24/2019] [Revised: 12/30/2019] [Accepted: 01/16/2020] [Indexed: 06/08/2023]
Abstract
A common assumption in tropical ecology is that root systems respond rapidly to climatic cues but that most of that response is limited to the uppermost layer of the soil, with relatively limited changes in deeper layers. However, this assumption has not been tested directly, preventing models from accurately predicting the response of tropical forests to environmental change.We measured seasonal dynamics of fine roots in an upper-slope plateau in Central Amazonia mature forest using minirhizotrons to 90 cm depth, which were calibrated with fine roots extracted from soil cores.Root productivity and mortality in surface soil layers were positively correlated with precipitation, whereas root standing length was greater during the dry periods at the deeper layers. Contrary to historical assumptions, a large fraction of fine-root standing biomass (46%) and productivity (41%) was found in soil layers deeper than 30 cm. Furthermore, root turnover decreased linearly with soil depth.Our findings demonstrate a relationship between fine-root dynamics and precipitation regimes in Central Amazonia. Our results also emphasize the importance of deeper roots for accurate estimates of primary productivity and the interaction between roots and carbon, water, and nutrients.
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Affiliation(s)
- Amanda L. Cordeiro
- Instituto Nacional de Pesquisas da Amazônia – INPAManausBrazil
- Colorado State University – CSUFort CollinsCOUSA
| | | | | | - Oscar Valverde‐Barrantes
- Instituto Nacional de Pesquisas da Amazônia – INPAManausBrazil
- Florida International University –MiamiMiamiFLUSA
| | - Lucia Fuchslueger
- Instituto Nacional de Pesquisas da Amazônia – INPAManausBrazil
- University of AntwerpAntwerpBelgium
| | - Erick Oblitas
- Instituto Nacional de Pesquisas da Amazônia – INPAManausBrazil
| | - Iain P. Hartley
- GeographyCollege of Life and Environmental SciencesUniversity of ExeterExeterUK
| | | | - Nathan B. Gonçalves
- Instituto Nacional de Pesquisas da Amazônia – INPAManausBrazil
- Michigan State University – MSUEast LansingMIUSA
| | - Bruno Takeshi
- Instituto Nacional de Pesquisas da Amazônia – INPAManausBrazil
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