
Boletín del Centro de Investigaciones Biológicas
Vol. 59. N.º 1, Enero-Junio 2025, Pp. 12-32
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(Biebl and Kinzel 1965, Medina and Francisco 1997, Sobrado 2004, Méndez-Alonzo
et al. 2016), reporting until 1650 mmol/Kg at 40 ‰ in coastal lagoons (Medina and
Francisco 1997). Cardona Olarte et al. (2006), demonstrated that cultivated seedlings
grow better at a salinity of 10 ‰, with alternating flooding, however Lonard et al.
2021, found that the optimal conditions for growth under natural environment are
nutrient-rich soils and moderate salinity (15 – 20 ‰).
Biebl and Kinzel (1965) early on they argued that salinity tolerance of this species
is based on the development of leaf succulence, compensating ion accumulation in
vacuoles through dilution, combined with and the active secretion of salt by leaf glands
(Sobrado 2004, Francisco et al. 2009, Quadros et al. 2021).
Among mangrove species, L. racemosa is characterized by higher Ca leaf
concentrations (Barboza et al. 2006, Madi et al. 2015, Medina et al. 2015 a, b).
Calcium is an element essential for the maintenance of membrane permeability at the
root level, and for the structural stability of shoots and roots through the formation of
Ca pectates gluing together cell walls (Marschner 1995, White and Broadley 2003,
Hirschi 2004). Nitrogen and phosphorous have been identified as limiting nutrients for
structural development of mangrove ecosystems throughout the world (Feller 1995,
Chen and Twilley 1999, McKee et al. 2002, Lovelock et al. 2006). It has been shown
in non-halophytes that Na ions inhibit competitively the uptake of K, Mg, and Ca,
whereas the high levels of Cl ions may reduce the uptake of PO4 and NO3 (Lu and
Fricke 2023). These effects of salinity on nutrient uptake may differ in mangroves, as
they display various mechanisms regulating Na accumulation such as reduced uptake
through the roots, leaf succulence, and salt glands (Ball et al. 1987, Parida and Jha
2010). Several authors consider them as obligate halophytes (Wang et al. 2011), but in
this study is prefer to describe as salt tolerant, along the lines discussed by Barbour
(1970), Grigori et al. (2012) and Krauss and Ball (2013). However, the mangrove
species show large differences in cations accumulation and salinity tolerance in the
field (Medina et al. 2015b).
In the present study is quantified, under semi-controlled conditions, the effect of
salinity on a) the biomas production and distribution into leaves, stems, and roots; b)
the diurnal variations in osmolality and ionic composition of leaf sap; c) the
fractionation of Ca in leaves; d) the nutrients uptake and allocation by cultivated