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1.
Plants (Basel) ; 13(11)2024 May 30.
Article in English | MEDLINE | ID: mdl-38891311

ABSTRACT

Roots play a fundamental role in forest ecosystems, but obtaining samples from deep layers remains a challenging process due to the methodological and financial efforts required. In our quest to understand the dynamics of Eucalyptus roots, we raise three fundamental questions. First, we inquire about the average extent of the roots of two contrasting Eucalyptus genotypes. Next, we explore the factors that directly influence the growth and depth of these roots, addressing elements such as soil type, climate, and water availability. Lastly, we investigate how the variation in Eucalyptus species may impact root growth patterns, biomass, and carbon stock. In this study, we observed that the maximum root depth increased by an average of 20% when genotypes were grown on sites with higher water availability (wet site). E. urophylla stands had a higher biomass and carbon stock (5.7 Mg C ha-1) of fine roots when cultivated on dry sites (annual rainfall~727 mm) than the wet sites (annual rainfall~1590 mm). In E. grandis × E. camaldulensis stands, no significant differences were observed in the stock of fine root biomass (3.2 Mg C ha-1) between the studied environments. Our results demonstrated that genotypes with greater drought tolerance (E. grandis × E. camaldulensis) tend to maintain higher stocks of fine root biomass (3.2-6.3 Mg ha-1) compared to those classified as plastic (E. urophylla), regardless of the edaphoclimatic conditions of the cultivation site. Finally, our research helps understand how Eucalyptus trees adapt to their environment, aiding sustainable forest management and climate change mitigation. We also provide a practical tool to estimate underground biomass, assisting forest managers and policymakers in ensuring long-term forest sustainability.

2.
Theor Appl Climatol ; 149(3-4): 1431-1450, 2022.
Article in English | MEDLINE | ID: mdl-35756150

ABSTRACT

Many regions around the world are facing climate changes, with substantial increase in air temperature over the past decades, which is mainly related to continental and global warming forced by the higher greenhouse gas (GHG) emissions. The objectives of this study were to use the Köppen climate classification to detect local climate change based on a historical series of 100 years and to assess if such change is related to those that are occurring in other spatial scales as a likely consequence of increasing GHG. This paper brings a content full of innovative results. The study area presented an average annual air temperature increase by 0.9 °C between 1917 and 2016, rising from 21.4 °C for the first climatological normal (1917-1946) to 22.3 °C for the last one (1987-2016). Furthermore, in the summer months, the temperature rose from 24.5 to 25.3 °C, and in the winter months, such increase was from 17.1 (1917-1946) to 18.3 °C (1987-2016). Our findings showed the subtropical conditions (Cfa in Köppen's classification) in the study area persisted from the beginning of the analysis (1917-1946) until the climatological normal of 1979-2008, with a clear tendency of tropicalization after that with a change in the climate type of Piracicaba from subtropical to tropical, which can now be classified as tropical with dry winter (Aw climate type). The local average air temperature showed concordances with the long-term air temperature anomalies from regional, continental, and global scales, indicating that all of them may be linked with increasing GHG emissions, since well-defined long-term linear relationships (r 2 = 0.99) were observed between continental and global average air temperature anomalies and atmospheric CO2 concentration observed at the NOAA Lab in Mauna Loa in the last 59 years. While the local and regional forcing effects remain to be fully unraveled, our study provided a valid and strong scientific sound evidence that climate change occurred in Piracicaba, southeastern Brazil, in the last 100 years.

3.
Arq. Inst. Biol ; 82: 1-6, 2015. tab, mapas, graf
Article in Portuguese | LILACS, VETINDEX | ID: biblio-1026505

ABSTRACT

Entre janeiro e fevereiro de 2013 ocorreu uma epidemia de mal das folhas em regiões consideradas como de "escape" à doença, causando preocupações e indagações nos produtores de borracha e ao setor heveícola como um todo. Uma possível adaptação do fungo a essas zonas foi levantada e a consistência do controle da doença pela utilização do binômio plantas com troca uniforme das folhas + período seco, típicos de regiões de "escape", foi questionada. O objetivo deste trabalho foi trazer informações importantes aos heveicultores sobre a interação clima-patógeno-hospedeiro e comparar variáveis de normais climatológicas (média histórica) e dados climáticos deste período de ocorrência da epidemia (janeiro e fevereiro de 2013). Concluiu-se que não foi o patógeno que se adaptou às plantas de seringueira em clima mais seco, nas regiões de "escape", mas que o clima mais úmido ocorreu nessas regiões mais secas, nesse período.(AU)


In January and February 2013 occurred a South American leaf blight epidemic in regions considered as escape zones, causing concern to rubber tree growers and throughout the rubber industry. A possible adaptation of the fungus to escape zones was raised and the consistency of disease control by the use of the binomial: plants with uniform renewal of leaves + dry season, typical of the escape zones, was questioned. The aim of this work was to bring relevant information to the rubber growers about the interaction climate-pathogen-host and to compare normal climate (historical average) and climatic data of the occurrence period of epidemic (January and February 2013). We conclude that was not the pathogen that has adapted to rubber tree in drier conditions, typical in escape regions, but a more humid climate occurred in these drier regions during this period.(AU)


Subject(s)
Pest Control , Climate , Hevea/microbiology , Epidemics , Noxae , Dry Season
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