The onset of xylogenesis is not related to distance from the crown in Smith fir trees from the southeastern Tibetan Plateau

2016 ◽  
Vol 46 (6) ◽  
pp. 885-889 ◽  
Author(s):  
Xiaoxia Li ◽  
J. Julio Camarero ◽  
Bradley Case ◽  
Eryuan Liang ◽  
Sergio Rossi

Young and mature trees are usually characterized by asynchronous growth resumption of xylem. Here, we test the hypothesis that the later onset of xylem growth in older trees is related to the longer distance of the stem from the developing buds, which represents the main source of hormones triggering vascular tissue differentiation. We compared the onset of xylogenesis at different heights along the stems of young and mature Smith fir (Abies georgei var. smithii (Viguie & Gaussen) W. C. Cheng & L. K. Fu)) trees in the Sygera Mountains, southeastern Tibetan Plateau. Xylem formation was monitored weekly in 2012 on anatomical sections of wood microcores. The onset of xylogenesis differed between young and mature trees, with most phases occurring 2 weeks later in mature trees. No effect of the sampling height was observed on the growth resumption. Our results suggest that the later resumption of xylogenesis in older conifer trees is not related to their longer distance from the crown.

2021 ◽  
Vol 811 ◽  
pp. 228871
Author(s):  
Chengyu Zhu ◽  
Guocan Wang ◽  
Philippe Hervé Leloup ◽  
Kai Cao ◽  
Gweltaz Mahéo ◽  
...  

2021 ◽  
Vol 12 (1) ◽  
Author(s):  
Maoliang Zhang ◽  
Zhengfu Guo ◽  
Sheng Xu ◽  
Peter H. Barry ◽  
Yuji Sano ◽  
...  

AbstractThe episodic growth of high-elevation orogenic plateaux is controlled by a series of geodynamic processes. However, determining the underlying mechanisms that drive plateau growth dynamics over geological history and constraining the depths at which growth originates, remains challenging. Here we present He-CO2-N2 systematics of hydrothermal fluids that reveal the existence of a lithospheric-scale fault system in the southeastern Tibetan Plateau, whereby multi-stage plateau growth occurred in the geological past and continues to the present. He isotopes provide unambiguous evidence for the involvement of mantle-scale dynamics in lateral expansion and localized surface uplift of the Tibetan Plateau. The excellent correlation between 3He/4He values and strain rates, along the strike of Indian indentation into Asia, suggests non-uniform distribution of stresses between the plateau boundary and interior, which modulate southeastward growth of the Tibetan Plateau within the context of India-Asia convergence. Our results demonstrate that deeply-sourced volatile geochemistry can be used to constrain deep dynamic processes involved in orogenic plateau growth.


2018 ◽  
Vol 123 (11) ◽  
pp. 9733-9749 ◽  
Author(s):  
Tuo Zheng ◽  
Zhifeng Ding ◽  
Jieyuan Ning ◽  
Lijun Chang ◽  
Xingchen Wang ◽  
...  

2013 ◽  
Vol 104 ◽  
pp. 23-33 ◽  
Author(s):  
Xiaohong Liu ◽  
Xiaomin Zeng ◽  
Steven W. Leavitt ◽  
Wenzhi Wang ◽  
Wenling An ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document