Abstract

The Three-North Shelter Forest (TNSF) is a critical ecological barrier against sandstorms in northern China, but has shown extensive decline and death in Populus simonii Carr. in the last decade. We investigated the characteristics—tree-ring width, basal area increment (BAI), carbon isotope signature (13Ccor), and intrinsic water-use efficiency (iWUE)—of now-dead, dieback, and non-dieback trees in TNSF shelterbelts of Zhangbei County. Results from the three groups were compared to understand the long-term process of preceding drought-induced death and to identify potential early-warning proxies of drought-triggered damage. The diameter at breast height (DBH) was found to decrease with the severity of dieback, showing an inverse relationship. In all three groups, both tree-ring width and BAI showed quadratic relationships with age, and peaks earlier in the now-dead and dieback groups than in the non-dieback group. The tree-ring width and BAI became significantly lower in the now-dead and dieback groups than in the non-dieback group from 17 to 26 years before death, thus, these parameters can serve as early-warning signals for future drought-induced death. The now-dead and dieback groups had significantly higher δ13Ccor and iWUEs than the non-dieback group at 7–16 years prior to the mortality, indicating a more conservative water-use strategy under drought stress compared with non-dieback trees, possibly at the cost of canopy defoliation and long-term shoot dieback. The iWUE became significantly higher in the now-dead group than in the dieback group at 0–7 years before death, about 10 years later than the divergence of BAI. After the iWUE became significantly different among the groups, the now-dead trees showed lower growth and died over the next few years. This indicates that, for the TNSF shelterbelts studied, an abrupt iWUE increase can be used as a warning signal for acceleration of impending drought-induced tree death. In general, we found that long-term drought decreased growth and increased iWUE of poplar tree. Successive droughts could drive dieback and now-dead trees to their physiological limits of drought tolerance, potentially leading to decline and mortality episodes.

Highlights

  • Drought-induced plant mortality is increasing globally as the earth continues to warm

  • The intrinsic water-use efficiency (iWUE) of all three balance (ET0 –P) in August (p < 0.05). These results indicated that, compared with tree-ring width and groups was significantly correlated with precipitation, temperature, relative humidity, ET0, and basal area increment (BAI), iWUE was more sensitive to environmental factors

  • During the entire growing season, water balance (ET0–P) in August (p < 0.05). These results indicated that, compared with tree-ring the environmental factors in August played a key role in the water use of poplar trees

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Summary

Introduction

Drought-induced plant mortality is increasing globally as the earth continues to warm. Drought-induced tree death has been recognized as an important ecological issue It is not fully understood why some trees survive drought effectively while other coexisting individuals do not [3]. This insufficient understanding has stimulated investigation into the mechanisms of plant death by hydraulic failure [4,5], carbon starvation [6], and biological attack [3,7,8]. In response to water deficit, trees limit their vigor or growth, leading to their decline. To better characterize this phenomenon, the long period of growth before drought-induced tree death needs to be quantified by new approaches. Other studies have reported that comparison of past radial growth trends among dead, dieback (severely defoliated), and non-dieback (slightly or not defoliated) trees may help to identify early warning signals of drought-triggered mortality [13,14]

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