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  • 1
    Publication Date: 2015-11-26
    Description: Drought threatens tropical rainforests over seasonal to decadal timescales, but the drivers of tree mortality following drought remain poorly understood. It has been suggested that reduced availability of non-structural carbohydrates (NSC) critically increases mortality risk through insufficient carbon supply to metabolism ('carbon starvation'). However, little is known about how NSC stores are affected by drought, especially over the long term, and whether they are more important than hydraulic processes in determining drought-induced mortality. Using data from the world's longest-running experimental drought study in tropical rainforest (in the Brazilian Amazon), we test whether carbon starvation or deterioration of the water-conducting pathways from soil to leaf trigger tree mortality. Biomass loss from mortality in the experimentally droughted forest increased substantially after 〉10 years of reduced soil moisture availability. The mortality signal was dominated by the death of large trees, which were at a much greater risk of hydraulic deterioration than smaller trees. However, we find no evidence that the droughted trees suffered carbon starvation, as their NSC concentrations were similar to those of non-droughted trees, and growth rates did not decline in either living or dying trees. Our results indicate that hydraulics, rather than carbon starvation, triggers tree death from drought in tropical rainforest.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Rowland, L -- da Costa, A C L -- Galbraith, D R -- Oliveira, R S -- Binks, O J -- Oliveira, A A R -- Pullen, A M -- Doughty, C E -- Metcalfe, D B -- Vasconcelos, S S -- Ferreira, L V -- Malhi, Y -- Grace, J -- Mencuccini, M -- Meir, P -- England -- Nature. 2015 Dec 3;528(7580):119-22. doi: 10.1038/nature15539. Epub 2015 Nov 23.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of GeoSciences, University of Edinburgh, Edinburgh EH9 3FF, UK. ; Centro de Geosciencias, Universidade Federal do Para, Belem 66075-110, Brazil. ; School of Geography, University of Leeds, Leeds LS2 9JT, UK. ; Instituto de Biologia, UNICAMP, Campinas 13.083-970, Brazil. ; The University of Cambridge, Cambridge CB2 1TN, UK. ; Environmental Change Institute, The University of Oxford, Oxford OX1 3QY, UK. ; Department of Physical Geography and Ecosystem Science, Lund University, Lund S-223 62, Sweden. ; EMBRAPA Amazonia Oriental, Belem 66095-903, Brazil. ; Museu Paraense Emilio Goeldi, Belem 66077-830, Brazil. ; ICREA at CREAF, 08193 Cerdanyola del Valles, Spain. ; Research School of Biology, Australian National University, Canberra, Australian Capital Territory 2601, Australia.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26595275" target="_blank"〉PubMed〈/a〉
    Keywords: Biomass ; Body Size ; Brazil ; Carbohydrate Metabolism ; Carbon/*metabolism ; *Droughts ; Plant Leaves/metabolism ; Plant Stems/metabolism ; *Rainforest ; Seasons ; Soil/chemistry ; Trees/growth & development/*metabolism ; *Tropical Climate ; Water/*metabolism ; Xylem/metabolism
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2014-02-07
    Description: Feedbacks between land carbon pools and climate provide one of the largest sources of uncertainty in our predictions of global climate. Estimates of the sensitivity of the terrestrial carbon budget to climate anomalies in the tropics and the identification of the mechanisms responsible for feedback effects remain uncertain. The Amazon basin stores a vast amount of carbon, and has experienced increasingly higher temperatures and more frequent floods and droughts over the past two decades. Here we report seasonal and annual carbon balances across the Amazon basin, based on carbon dioxide and carbon monoxide measurements for the anomalously dry and wet years 2010 and 2011, respectively. We find that the Amazon basin lost 0.48 +/- 0.18 petagrams of carbon per year (Pg C yr(-1)) during the dry year but was carbon neutral (0.06 +/- 0.1 Pg C yr(-1)) during the wet year. Taking into account carbon losses from fire by using carbon monoxide measurements, we derived the basin net biome exchange (that is, the carbon flux between the non-burned forest and the atmosphere) revealing that during the dry year, vegetation was carbon neutral. During the wet year, vegetation was a net carbon sink of 0.25 +/- 0.14 Pg C yr(-1), which is roughly consistent with the mean long-term intact-forest biomass sink of 0.39 +/- 0.10 Pg C yr(-1) previously estimated from forest censuses. Observations from Amazonian forest plots suggest the suppression of photosynthesis during drought as the primary cause for the 2010 sink neutralization. Overall, our results suggest that moisture has an important role in determining the Amazonian carbon balance. If the recent trend of increasing precipitation extremes persists, the Amazon may become an increasing carbon source as a result of both emissions from fires and the suppression of net biome exchange by drought.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gatti, L V -- Gloor, M -- Miller, J B -- Doughty, C E -- Malhi, Y -- Domingues, L G -- Basso, L S -- Martinewski, A -- Correia, C S C -- Borges, V F -- Freitas, S -- Braz, R -- Anderson, L O -- Rocha, H -- Grace, J -- Phillips, O L -- Lloyd, J -- England -- Nature. 2014 Feb 6;506(7486):76-80. doi: 10.1038/nature12957.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Instituto de Pesquisas Energeticas e Nucleares (IPEN)-Comissao Nacional de Energia Nuclear (CNEN)-Atmospheric Chemistry Laboratory, 2242 Avenida Professor Lineu Prestes, Cidade Universitaria, Sao Paulo CEP 05508-000, Brazil [2]. ; 1] School of Geography, University of Leeds, Woodhouse Lane, Leeds LS9 2JT, UK [2]. ; 1] Global Monitoring Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80305, USA [2] Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, Colorado 80309, USA [3]. ; Environmental Change Institute, School of Geography and the Environment, University of Oxford, South Parks Road, Oxford OX1 3QY, UK. ; Instituto de Pesquisas Energeticas e Nucleares (IPEN)-Comissao Nacional de Energia Nuclear (CNEN)-Atmospheric Chemistry Laboratory, 2242 Avenida Professor Lineu Prestes, Cidade Universitaria, Sao Paulo CEP 05508-000, Brazil. ; Center for Weather Forecasts and Climate Studies, Instituto Nacional de Pesquisas Espaciais (INPE), Rodovia Dutra, km 39, Cachoeira Paulista CEP 12630-000, Brazil. ; 1] Environmental Change Institute, School of Geography and the Environment, University of Oxford, South Parks Road, Oxford OX1 3QY, UK [2] Remote Sensing Division, INPE (National Institute for Space Research), 1758 Avenida dos Astronautas, Sao Jose dos Campos CEP 12227-010, Brazil. ; Departamento de Ciencias Atmosfericas/Instituto de Astronomia e Geofisica (IAG)/Universidade de Sao Paulo, 1226 Rua do Matao, Cidade Universitaria, Sao Paulo CEP 05508-090, Brazil. ; Crew Building, The King's Buildings, West Mains Road, Edinburgh EH9 3JN, UK. ; School of Geography, University of Leeds, Woodhouse Lane, Leeds LS9 2JT, UK. ; 1] School of Tropical and Marine Biology and Centre for Terrestrial Environmental and Sustainability Sciences, James Cook University, Cairns 4870, Queensland, Australia [2] Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, Berkshire, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24499918" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Biomass ; Biota ; Brazil ; *Carbon Cycle ; Carbon Dioxide/analysis ; Carbon Monoxide/analysis ; Droughts/*statistics & numerical data ; Fires/statistics & numerical data ; Fresh Water/analysis ; Photosynthesis ; Rain ; Seasons ; Trees/metabolism ; Tropical Climate
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Planta 202 (1997), S. 455-461 
    ISSN: 1432-2048
    Keywords: Key words: Cohesion theory ; Linear variable displa cement transducer ; Modulus of elasticity ; Pinus ; Water potential
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract. According to the cohesion theory for the ascent of water in vascular plants, significant tensions should develop in the water columns of transpiring trees. These tensions cause small but detectable changes in the diameter of the xylem as a consequence of adhesive forces between water molecules and the inner xylem walls. The diurnal time course of tension in the water columns in the xylem of the trunk of mature Scots pine (Pinus sylvestris L.) was measured during the summer of 1995 by means of a displacement transducer mounted on a rigid steel frame. The apparent elastic modulus of Scots pine wood in the radial direction (E  ′ r ) was determined in the laboratory and then used to estimate tensions from the measured displacement. Laboratory measurements on logs indicated that only the sapwood contributed to dimensional changes of the xylem. Corrections for thermal expansion of the system were included. Water tensions fell by 0.19 MPa over the course of the day, when needle water potentials fell by 0.50 MPa. Such data are consistent with the cohesion theory, and with the view that the hydraulic resistances to flow in above- and below-ground plant parts are of similar magnitude.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1573-5052
    Keywords: Acoustic emissions ; Cavitation ; Heather ; Relative water content ; Stomatal conductance ; Water potential
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The acoustic emission rate (as a result of xylem cavitation), stem water content, stomatal conductance, and leaf water potential of heather (Calluna vulgaris L. Hull) were compared over a period of 18 months at two contrasting sites in Britain. The sites were Thursely Common in south-east England, and Flanders Moss in central Scotland (average rainfall of 600 mm per year and 1500 mm per year, respectively). In the first year of study (1992) the natural difference between the sites was amplified by a severe drought affecting south-east England. The relative water content of the xylem (RWC) did not differ between the sites, and did not fluctuate seasonally, despite the drought at Thursely. Acoustic emissions were detected at both sites, but the incidence was low. The same range of foliage water potential and stomatal conductance was found at both sites. The leaf area to sapwood area ratio at the dry site was half that at the wet site, and it is suggested that this adjustment of the transpiring area relative to the water conducting area facilitates the close physiological state of the plants at the two sites. The possible occurrence of aerial refilling and freezing induced xylem cavitation is also discussed.
    Type of Medium: Electronic Resource
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