Evaluation of the effect of the 2011 Tsunami on coastal forests by means of multiple isotopic analyses of tree-rings. Issue 5 (3rd September 2018)

• Record Type: Journal Article
• Authors: Lopez Caceres, Maximo Larry; Nakano, Sayako; Ferrio, Juan Pedro; Hayashi, Mika; Nakatsuka, Takeshi; Sano, Masaki; Yamanaka, Toshiro; Nobori, Yoshihiro
• Is Part Of: Isotopes in environmental and health studies. Volume 54:Issue 5(2018)
• Page Start: 494
• Page End: 507
• Publication Date: 2018-09-03
• Subjects: Carbon-13 -- coastal forests -- isotope ecology -- nitrogen-15 -- oxygen-18 -- soil salinity -- tsunami -- tree-rings; Isotopes -- Periodicals; Radioisotopes -- Periodicals; Environment -- Periodicals; Isotopes -- Periodicals; Medicine -- Periodicals; Radioisotopes -- Periodicals; 541.388
• DOI: 10.1080/10256016.2018.1495203
• Languages: English
• ISSNs: 1025-6016

Abstract

ABSTRACT: 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 (δ 13 C, δ 15 N and δ 18 O). 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 δ 13 C. Sea water deposition in the soil did not affect tree-ring δ 18 O values. Two years after the tsunami, decreasing tree-ring δ 13 C 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 δ 13 C-δ 18 O model explains neither the limited growth nor the subsequent recovery in δ 13 C. Similarly tree-ring δ 15 N 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.