scholarly journals Spatiotemporal Variability in the Climate Growth Response of High Elevation Bristlecone Pine in the White Mountains of California

2018 ◽  
Vol 45 (24) ◽  
Author(s):  
Andrew G. Bunn ◽  
Matthew W. Salzer ◽  
Kevin J. Anchukaitis ◽  
Jamis M. Bruening ◽  
Malcolm K. Hughes
2001 ◽  
Vol 79 (3) ◽  
pp. 293-299 ◽  
Author(s):  
M I Bidartondo ◽  
J Baar ◽  
T D Bruns

Intersite variation in ectomycorrhizal (ECM) inoculum potential in soils from 16 sites located in arid subalpine areas of the White Mountains of California was quantified. The study sites included valleys dominated by big sagebrush (Artemisia tridentata Nutt.) and mountainsides dominated by ancient Great Basin bristlecone pine (Pinus longaeva Bailey). ECM inoculum potential was not detected at three of four valley sites nor in 42% of forest soil samples. Only 10 mycorrhizal species were detected in bioassays, and four of those accounted for 94.5% of all colonized seedlings, in order of decreasing abundance these were Pyronemataceae sp., Rhizopogon sp., Wilcoxina rehmii Yang & Korf, and Cenococcum sp. These species were identified also from in situ mycorrhizal roots. The abundance of the dominant Pyronemataceae sp. was significantly positively correlated with pH, which at all forest sites was high compared with typical conifer forest soils. Our results show that the ECM inoculum potential of soils is low, homogeneous, and spatially restricted in these ancient high-elevation forests.Key words: fungal community, molecular ecology, spore dispersal.


2020 ◽  
Author(s):  
Laura Dye ◽  
◽  
Cori Butkiewicz ◽  
Zane Cooper ◽  
Bethany Coulthard ◽  
...  

Ecosphere ◽  
2021 ◽  
Vol 12 (7) ◽  
Author(s):  
Keridwen M. Whitmore ◽  
Nehemiah Stewart ◽  
Andrea C. Encalada ◽  
Esteban Suárez ◽  
Diego A. Riveros‐Iregui

1973 ◽  
Vol 3 (4) ◽  
pp. 632-660 ◽  
Author(s):  
Valmore C. LaMarche

AbstractRemains of dead bristlecone pine (Pinus longaeva Bailey) are found at altitudes up to 150 m above present treeline in the White Mountains. Standing snags and remnants in two study areas were mapped and sampled for dating by tree-ring and radiocarbon methods. The oldest remnants represent trees established more than 7400 y.a. Experimental and empirical evidence indicates that the position of the treeline is closely related to warm-season temperatures, but that precipitation may also be important in at least one of the areas. The upper treeline was at high levels in both areas until after about 2200 B.C., indicating warm-season temperatures about 3.5°F higher than those of the past few hundred years. However, the record is incomplete, relative warmth may have been maintained until at least 1500 B.C. Cooler and wetter conditions are indicated for the period 1500 B.C.-500 B.C., followed by a period of cool but drier climate. A major treeline decline occurred between about A.D. 1100 and A.D. 1500, probably reflecting onset of cold and dry conditions. High reproduction rates and establishment of scattered seedlings at high altitudes within the past 100 yr represents an incipient treeline advance, which reflected a general climatic warming beginning in the mid-19th century that has lasted until recent decades in the western United States. This evidence for climatic variation is broadly consistent with the record of Neoglacial advances in the North American Cordillera, and supports Antevs' concept of a warm “altithermal age” in the Great Basin.


2011 ◽  
Vol 76 (1) ◽  
pp. 22-29 ◽  
Author(s):  
Roderick J. Bale ◽  
Iain Robertson ◽  
Matthew W. Salzer ◽  
Neil J. Loader ◽  
Steven W. Leavitt ◽  
...  

AbstractWe present the first near millennium-length, annually resolved stable isotope record from bristlecone pines (Pinus longaeva, D.K Bailey). The carbon isotope ratios from the cellulose of seven trees from the White Mountains of California, corrected for anthropogenic changes in atmospheric chemistry, are used to reconstruct growing season (June through August) precipitation back to AD 1085. Extremely negative isotope results are strongly correlated with proposed severest El Niño events over the last 500 yr, and similar values in the first half of the millennium are used to reconstruct a further 13 strong El Niño events, concentrated in the 12th Century and the mid 13th and 14th Centuries. Ring-width chronologies from adjacent sites in the White Mountains demonstrate a high degree of decadal covariance with the δ13C series, although there are several periods of notable divergence.


1970 ◽  
Vol 2 (3) ◽  
pp. 227
Author(s):  
Waldo S. Glock ◽  
Paula V. Krebs ◽  
Harold C. Fritts

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