Long-term c i  / c a response of trees in western North America to atmospheric CO 2 concentration derived from carbon isotope chronologies

Oecologia ◽  
1998 ◽  
Vol 117 (1-2) ◽  
pp. 19-25 ◽  
Author(s):  
Xiahong Feng
1993 ◽  
Vol 130 (4) ◽  
pp. 443-452 ◽  
Author(s):  
R. L. Ripperdan ◽  
M. Magaritz ◽  
J. L. Kirschvink

AbstractCarbon isotope and magnetic polarity stratigraphic results from the Cambrian-Ordovician Boundary section at Xiaoyangqiao, near Dayangcha, Jilin Province, China, in comparison to a contemporaneous section at Black Mountain, Australia, indicate strata equivalent to major portions of the Australian sequence are either absent or are restricted to highly condensed intervals. These intervals are correlative with regressive sea level events identified in Australia and western North America, suggesting regional or eustatic sea level changes strongly influenced deposition of the Xiaoyangqiao sequence. These results also suggest the Xiaoyangqiao section is unfavourable as the site of the Cambrian-Ordovician Boundary Global Stratotype Section and Point.


The Condor ◽  
1991 ◽  
Vol 93 (1) ◽  
pp. 130-137 ◽  
Author(s):  
Leonard A. Brennan ◽  
Michael L. Morrison

2019 ◽  
Vol 15 (6) ◽  
pp. 20190011 ◽  
Author(s):  
Jesse L. Morris ◽  
R. Justin DeRose ◽  
Thomas Brussel ◽  
Simon Brewer ◽  
Andrea Brunelle ◽  
...  

As important centres for biological diversity, aspen forests are essential to the function and aesthetics of montane ecosystems in western North America. Aspen stands are maintained by a nuanced relationship with wildfire, although in recent decades aspen mortality has increased. The need to understand the baseline environmental conditions that favour aspen is clear; however, long-term fire history reconstructions are rare due to the scarcity of natural archives in dry montane settings. Here, we analyse a high-resolution lake sediment record from southwestern, Utah, USA to quantify the compositional and burning conditions that promote stable (or seral) aspen forests. Our results show that aspen presence is negatively correlated with subalpine fir and that severe fires tend to promote persistent and diverse aspen ecosystems over centennial timescales. This information improves our understanding of aspen disturbance ecology and identifies the circumstances where critical transitions in montane forests may occur.


The Condor ◽  
10.1650/7131 ◽  
2003 ◽  
Vol 105 (4) ◽  
pp. 737 ◽  
Author(s):  
Grant Ballard ◽  
Geoffrey R. Geupel ◽  
Nadav Nur ◽  
Thomas Gardali

Sign in / Sign up

Export Citation Format

Share Document