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Vol.:(0123456789)
1 3
Planta (2019) 250:1011–1032
https://doi.org/10.1007/s00425-019-03220-4
REVIEW
Boron toxicity inhigher plants: anupdate
MarcoLandi1· TheoniMargaritopoulou2· IoannisE.Papadakis3 · FabrizioAraniti4
Received: 27 March 2019 / Accepted: 18 June 2019 / Published online: 24 June 2019
© Springer-Verlag GmbH Germany, part of Springer Nature 2019
Abstract
Main conclusion In this review, emphasis is given to the most recent updates about morpho-anatomical, physiologi-
cal, biochemical and molecular responses adopted by plants to cope with B excess.
Abstract Boron (B) is a unique micronutrient for plants given that the range of B concentration from its essentiality to
toxicity is extremely narrow, and also because it occurs as an uncharged molecule (boric acid) which can pass lipid bilayers
without any degree of controls, as occurs for other ionic nutrients. Boron frequently exceeds the plant’s requirement in arid
and semiarid environments due to poor drainage, and in agricultural soils close to coastal areas due to the intrusion of B-rich
seawater in fresh aquifer or because of dispersion of seawater aerosol. Global releases of elemental B through weathering,
volcanic and geothermal processes are also relevant in enriching B concentration in some areas. Considerable progress has
been made in understanding how plants react to B toxicity and relevant efforts have been made to investigate: (I) B uptake and
in planta partitioning, (II) physiological, biochemical, and molecular changes induced by B excess, with particular emphasis
to the effects on the photosynthetic process, the B-triggered oxidative stress and responses of the antioxidant apparatus to B
toxicity, and finally (III) mechanisms of B tolerance. Recent findings addressing the effects of B toxicity are reviewed here,
intending to clarify the effect of B excess and to propose new perspectives aimed at driving future researches on the topic.
Keywords Boric acid· Boron partitioning· Boron-polyol complexes· Boron tolerance· Boron transporter· Oxidative
stress
Introduction
Boron (B) toxicity limits crop yield and quality in several
agricultural areas worldwide, and frequently occurs naturally
in alkaline and saline soils together with a low rainfall and
very scarce leaching (Camacho-Cristóbal etal. 2018; Landi
etal. 2012), in agricultural lands close to coastal area (Kabay
etal. 2010) or in areas with persistent geothermal activities
(Princi etal. 2016a). Indeed, ocean evaporation is the pre-
dominant source of B release in the biosphere (65–85%),
whereas natural chemical and mechanical weathering of
sedimentary rocks provide B compounds in soil and water
(Princi etal. 2016a). The most impactful source of highly
concentrated B, with an average of 5–6mg B l−1 (Kabay
etal. 2010), is certainly the seawater, whose intrusion occurs
naturally in most coastal aquifers, owing to the hydraulic
connection between groundwater and seawater, thereby
increasing B concentration in irrigation water (Reid 2010).
Differently to other pollutants, environmental B release
that is directly or indirectly attributable to human activi-
ties plays a minor role compared to the amplitude of the
environmental B-enrichment deriving from natural sources.
List of anthropogenic sources based on their increased con-
tribution to B release worldwide is agriculture, wood burn-
ing, power generation from coal and oil, glass manufacture,
use of borates/perborates, borate mining and processing,
* Ioannis E. Papadakis
papadakis@aua.gr
1 Department ofAgriculture, Food andEnvironment,
University ofPisa, Via del Borghetto 80, 56124Pisa, Italy
2 Laboratory ofMycology, Department ofPhytopathology,
Benaki Phytopathological Institute, St. Delta 8,
14561Kifisia, Greece
3 Laboratory ofPomology, Department ofCrop Science,
Agricultural University ofAthens, Iera Odos 75,
11855Athens, Greece
4 Dipartimento AGRARIA, Università Mediterranea di Reggio
Calabria, Località Feo di Vito, SNC, 89124ReggioCalabria,
RC, Italy
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