Estimation of sulphate concentration in high elevation fog in Northeastern North America

2003 ◽  
Vol 37 (8) ◽  
pp. 1087-1100 ◽  
Author(s):  
Natty Urquizo ◽  
Jeffrey R Brook ◽  
John L Walmsley ◽  
William R Burrows
2000 ◽  
Vol 15 (4) ◽  
pp. 227-231 ◽  
Author(s):  
R.L. Livingston ◽  
J.E. Dewey ◽  
D.P. Beckman ◽  
L.E. Stipe

Abstract The balsam woolly adelgid (Adelges piceae) was introduced from Europe to northeastern North America in about 1900. In 1983, it was discovered infesting fir trees in Idaho. Since then, aerial and ground surveys have documented its spread in Idaho over an area of approximately 14,000 mi2 (8,960,000 ac). It now covers most of the central one-third of the state. Aerial surveys in 1997 and 1998 identified about 125,000 ac of host type with dead or damaged trees. Subalpine fir (Abies lasiocarpa) is a critical species in many high elevation areas. The effects of the balsam wooly adelgid on aesthetics, hydrology, and other ecological values can be very important. The adelgid is likely to continue its spread throughout subalpine fir forests of Idaho and neighboring states. West. J. Appl. For. 15(4):227-231,


1989 ◽  
Vol 19 (1) ◽  
pp. 145-148 ◽  
Author(s):  
Heiko Liedeker ◽  
Richard M. Klein

Characteristic spotting of foliage on Norway spruce in Europe, used as an indicator for Waldsterben, was also found and described on foliage of Piceaabies (L.) Karst., P. rubens Sarg., P. glauca (Moench) Voss, P. mariana (Mill.) B.S.P., Abiesbalsamea (L.) Mill., Pinusstrobus L., P. banksiana Lamb., P. resinosa Ait., P. sylvestris L., and Tsugacanadensis (L.) Carr. in northeastern North America. Yellow spotting is restricted to the upper, sun-exposed surface of the needles. These chlorotic spots generally start along ridges of the needles and merge into larger necrotic areas in later stages. It was observed that the number of spots per needle and the number of needles per internode exhibiting such spots are increasing with foliage age. The symptom was prominent on overstory and understory trees in high-elevation spruce–fir forests in Germany and northeastern North America. It was also found in all low-elevation stands sampled.


2019 ◽  
Author(s):  
Yiran Li ◽  
◽  
Vadim Levin ◽  
Zhenxin Xie

2021 ◽  
Vol 86 (2) ◽  
pp. 425-427
Author(s):  
John P. Hart ◽  
William A. Lovis ◽  
M. Anne Katzenberg

Emerson and colleagues (2020) provide new isotopic evidence on directly dated human bone from the Greater Cahokia region. They conclude that maize was not adopted in the region prior to AD 900. Placing this result within the larger context of maize histories in northeastern North America, they suggest that evidence from the lower Great Lakes and St. Lawrence River valley for earlier maize is “enigmatic” and “perplexing.” Here, we review that evidence, accumulated over the course of several decades, and question why Emerson and colleagues felt the need to offer opinions on that evidence without providing any new contradictory empirical evidence for the region.


2013 ◽  
Vol 20 (4) ◽  
pp. 559 ◽  
Author(s):  
Robert S. Capers ◽  
Kenneth D. Kimball ◽  
Kent P. McFarland ◽  
Michael T. Jones ◽  
Andrea H. Lloyd ◽  
...  

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