Juan Pedro Ferrio

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Blogs: 7
images: 17
Location: Zaragoza, Spain
Work interests: Plant Physiology, Forestry, Stable Isotopes, Archaeobotany, Agriculture, Plant breeding, Ecohydrology
Affiliation/website: https://www.juanpedroferrio.com
Preferred contact method: Any
Preferred contact language(s): English, Spanish
Contact: ARAID-Forest Resources Unit Agrifood Research and Technology Centre of Aragón (CITA) Avda. Montañana 930, 50059 Zaragoza, SPAIN
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Location: Lleida, Spain
Work: Plant ecophysiology, stable isotopes, archaeobotany, palaeoenvironment, plant breeding

Invitation to contribute to Special Issue "Stable Isotopes in Forest Ecosystem Research"
Deadline for submission: 31 May 2019

Dr. Juan Pedro Ferrio, ARAID-CITA, Spain
Prof. Dr. M. Larry Lopez C., Yamagata University, Japan
Guest Editors

I would like to draw your attention to a special issue on applications of stable isotopes in the journal Forests (MDPI, ISSN 1999-4907), which is now open for submission until 31st May 2019. We invite contributions on the use of SI in forest ecology and ecophysiology, including carbon, nutrient and water balance, and plant-plant and plant-microbial interactions, among others. We encourage potential authors to contact us in advance in order to ensure that the submission fits within the scope, as well as to solve any doubts about the submission process.

 


 

Special issue information:

Globally, forests are able to fix about 30% of annual anthropogenic CO2 emissions, and may be responsible for 70–90% of continental water losses. Therefore, understanding forest response to environmental drivers is crucial to anticipate and eventually mitigate the impacts of future global change. For this purpose, stable isotopes analysis has become a particularly suitable tool, offering time- and space-integrated information on the environmental effects on tree physiology and the implications for carbon, water and nutrient ecosystem balances. In this Special Issue, we invite studies developing applications of stable isotopes in forest ecology, tree physiology and ecohydrology, as well as modelling or empirical studies aimed at improving our mechanistic understanding of isotope fractionation in trees.

In particular, we encourage studies on the application of stables isotopes to the study of:

  • ecological interactions in relation to the use of resources, e.g. nutrients, water, light;
  • genetic variability in water uptake and water use efficiency in trees;
  • nutrient balance of forests in response to environmental or anthropogenic changes;
  • nitrogen dynamics: soil-mycorrhiza-plant interface;
  • interaction between forests and the hydrological cycle;
  • physiological response to different silvicultural treatments or disturbances;
  • whole-tree and ecosystem carbon and water balances;
  • validation and/or development of mechanistic models of isotope fractionation;
EVALUATION OF THE EFFECT OF THE 2011 TSUNAMI ON COASTAL FORESTS BY MEANS OF MULTIPLE ISOTOPIC ANALYSES OF TREE-RINGS


The March 2011 Mega-Tsunami in eastern Japan damaged at different degrees the black pine (Pinus thunbergii) forests along the coast. In order to evaluate the recovery of black pine four years later, tree-ring samples from 9 trees for the period 2002– 2014 were analyzed for ring growth and stable isotopes (δ13C, δ15N and δ18O). The results showed that annual tree-ring width decreased approximately 70 % from the year 2011 to 2014 compared to the period previous to the tsunami (2002–2010). The multiple isotopic analyses showed that the reduction in growth was caused by soil salinity that prompted stomatal closure and an abrupt increase of tree-ring δ13C. Sea water deposition in the soil did not affect tree-ring δ18O values. Two years after the tsunami, decreasing tree-ring δ13C values caused by apparently photosynthetic recovery did not translate into radial tree-growth, indicating a possible shift in carbon allocation to foliage and mainly roots as a defense mechanism to sodium toxicity. The dual δ13C-δ18O model explains neither the limited growth nor the subsequent recovery in δ13C. Similarly tree-ring δ15N indicated that there was no difference in nitrogen availability before and after the tsunami, suggesting that nutrients were not a limitation but rather soil salinity.

Máximo Larry López-Cáceres, Sayako Nakano, Juan Pedro Ferrio, Mika Hayashi, Takeshi Nakatsuka, Masaki Sano, Toshiro Yamanaka & Yoshihiro Nobori (2018) Evaluation of the effect of the 2011 Tsunami on coastal forests by means of multiple isotopic analyses of tree-rings. Isotopes in Environmental and Health Studies (In press) https://doi.org/10.1080/10256016.2018.1495203

URL: https://doi.org/10.1080/10256016.2018.1495203


HYDRAULIC CONSTRAINTS TO WHOLE-TREE WATER USE AND RESPIRATION IN YOUNG CRYPTOMERIA TREES UNDER COMPETITION

Although extensive studies have focused on carbon and water balance from aboveground measurements, the link between the belowground and aboveground processes deserves greater attention. In this context, the aim of this work was to assess the bi-directional feedback between whole-plant respiration and transpiration. The study was performed on 25 saplings of Sugi (Japanese cedar, Cryptomeria japonica D. Don), including dominant and suppressed individuals (total fresh weight ranging between 0.2 and 8.0 kg). During one week, the integrated water use (WU) was determined using the Deuterium dilution method. After this, the trees were uprooted and the root, stem, and leaf respiration were measured using incubation chambers and CO2 infrared sensors. The stem and root respiration followed a power response to mass (power exponent b < 1), implying a decline in mass-specific respiration with size. Conversely, the leaf respiration followed a near-linear increase with size (power exponent b ≈ 1), but was negatively affected by the stem density, indicating the hydraulic limitations of the leaf metabolism. The water use followed a power response with the tree size (b < 1), showing a decline in the transpiration per leaf mass with the tree size, but was also negatively correlated with the stem density. Our results indicate that dominant trees are more efficient in the use of water, and highlight the role of hydraulic limitations to leaf metabolism in suppressed trees.

 

Juan Pedro Ferrio, Yoko Kurosawa, Mofei Wang, Shigeta Mori (2018) Hydraulic Constraints to Whole-Tree Water Use and Respiration in Young Cryptomeria Trees under Competition. Forests 2018, 9(8), 449; https://doi.org/10.3390/f9080449


CONTRASTING ECOPHYSIOLOGICAL STRATEGIES RELATED TO DROUGHT: THE CASE OF A MIXED STAND OF SCOTS PINE (PINUS SYLVESTRIS) AND A SUBMEDITERRANEAN OAK (QUERCUS SUBPYRENAICA)

Submediterranean forests are considered an ecotone between Mediterranean and Eurosiberian ecosystems, and are very sensitive to global change. A decline of Scots pine (Pinus sylvestris L.) and a related expansion of oak species (Quercus spp.) have been reported in the Spanish Pre-Pyrenees. Although this has been associated with increasing drought stress, the underlying mechanisms are not fully understood, and suitable monitoring protocols are lacking. The aim of this study is to bring insight into the physiological mechanisms anticipating selective decline of the pines, with particular focus on carbon and water relations. For this purpose, we performed a sampling campaign covering two growing seasons in a mixed stand of P. sylvestris and Quercus subpyrenaica E.H del Villar. We sampled seasonally twig xylem and soil for water isotope composition (δ18O and δ2H), leaves for carbon isotope composition (δ13C) and stems to quantify non-structural carbohydrates (NSC) concentration, and measured water potential and leaf gas exchange. The first summer drought was severe for both species, reaching low predawn water potential (−2.2 MPa), very low stomatal conductance (12 ± 1.0 mmol m−2 s−1) and near-zero or even negative net photosynthesis, particularly in P. sylvestris (−0.6 ± 0.34 μmol m−2 s−1 in oaks, −1.3 ± 0.16 μmol m−2 s−1 in pines). Hence, the tighter stomatal control and more isohydric strategy of P. sylvestris resulted in larger limitations on carbon assimilation, and this was also reflected in carbon storage, showing twofold larger total NSC concentration in oaks than in pines (7.8 ± 2.4% and 4.0 ± 1.3%, respectively). We observed a faster recovery of predawn water potential after summer drought in Q. subpyrenaica than in P. sylvestris (−0.8 MPa and −1.1 MPa, respectively). As supported by the isotopic data, this was probably associated with a deeper and more reliable water supply in Q. subpyrenaica. In line with these short-term observations, we found a more pronounced negative effect of steadily increasing drought stress on long-term growth in pines compared with oaks. All these observations confer evidence of early warning of P. sylvestris decline and indicate the adaptive advantage of Q. subpyrenaica in the area.

Paula Martín-Gómez, Mònica Aguilera, Jesús Pemán, Eustaquio Gil-Pelegrín & Juan Pedro Ferrio (2017) Contrasting ecophysiological strategies related to drought: the case of a mixed stand of Scots pine (Pinus sylvestris) and a submediterranean oak (Quercus subpyrenaica). Tree Physiology, Volume 37, Issue 11, 1 November 2017, Pages 1478–1492

URL:  https://doi.org/10.1093/treephys/tpx101

Some minerals, like gypsum, hold water in their crystalline structure. The activation energy of the dehydration reaction of gypsum is relatively low and the conversion of gypsum to bassanite (CaSO4H2O) or anhydrite (CaSO4) may take place at ambient conditions. Although still unexplored, the use of such crystallization water by organisms would point to a completely new water source for life, critical under dry conditions.

In this study we analyzed the hydrogen (2H) and oxygen (18O) isotope composition of the xylem water of shallow-rooted plants growing on gypsum, and compared it to the isotopic composition of the free and crystallization water of the gypsum soils where they grow. According to our results, the isotopic composition of the xylem sap of plants was closer to gypsum crystallization water than to free soil water, particularly during the dry summer. Bayesian stable isotope mixing models indicated that gypsum crystallization water accounted for up to 90% of the water used bythese species during summer. Plants could also uptake gypsum crystallization water during spring, when itaccounted for up to 30% of the xylem sap of plants. Although the underlying mechanisms require further research, this is the first experimental evidence in support of the role of gypsum crystallization water as a water source for life. Our results change the current paradigm on water use by plants, where water held in the crystalline structure of mineral rocks is not regarded as a potential source. Given the existence of gypsum on the surface of Mars and its widespread occurrence on arid regions worldwide, these findings have important implications for exobiology, the study of life under extreme conditions and arid land reclamation.

http://blogs.egu.eu/geolog/2015/04/22/drinkable-rocks/

Palacio, S., Azorn, J., Montserrat-Mart, G. and Ferrio, J. P.: Drinkable rocks: plants can use crystallization water from gypsum. Geophysical Research Abstracts Vol. 17, EGU2015-9011-1, 2015

Palacio, S., Azorn, J., Montserrat-Mart, G. and Ferrio, J. P.: The crystallization water of gypsum rocks is a relevant water source for plants. Nature Communications,5, 2014

In this study we described the characteristics of agriculture at its beginnings by comparing kernel and wood samples from ancient Near East sites - the birthplace of Western agriculture -- with present day samples. It is the first time that direct evidences enable to know humidity and fertility conditions of crops, as well as the process of cereal domestication developed by humans from the Neolithic (12,000 years ago) to early Roman times (around 2,000 years ago).

Source:
Jos L. Araus, Juan P. Ferrio, Jordi Voltas, Mnica Aguilera, Ramn Bux. Agronomic conditions and crop evolution in ancient Near East agriculture. Nature Communications, 2014; 5 DOI: 10.1038/ncomms4953

I would like to draw your attention to our recent publication:

del Castillo J, Aguilera M, Voltas J, Ferrio JP (2013) Isoscapes of tree-ring carbon-13 perform like meteorological networks in predicting regional precipitation patterns. Journal of Geophysical Research Biogeosciences 118, 352-360

In this work, we managed to model spatial variability in mean annual precipitation from isotope data in a network of tree-ring sampling sites. Interestingly, the predictive ability of the models was almost identical to that obtained using a network of meteorological data with similar spatial density. This opens the possibility to upscale tree-ring reconstructions from local to regional levels.

Looking forward to getting your comments and suggestions about this study.

image014.gif?width=600

Figure: Comparison between A) annual precipitation according to the Atlas Climtico Digital de la Peninsula Ibrica (source: http://opengis.uab.es/wms/iberia/) and B) relative errors in isoscapes-estimated precipitation, based on the D13C of wood from Pinus halepensis and Quercus ilex (source: del Castillo et al. 2013).