Pitch Pine (Pinus rigida Mill.) Communities in the Hudson Valley Region of New York

1996 ◽  
Vol 136 (1) ◽  
pp. 42 ◽  
Author(s):  
Franz K. Seischab ◽  
John M. Bernard
1999 ◽  
Vol 29 (9) ◽  
pp. 1365-1373 ◽  
Author(s):  
R M Muzika ◽  
A M Liebhold

Ring widths from 1458 trees from Massachusetts, New York, and New Jersey were measured to determine the influence of gypsy moth (Lymantria dispar L.) defoliation on both hosts (primarily oaks (Quercus spp.)) and nonhosts. Previous year's defoliation negatively influenced radial increment in all oak species. Defoliation also negatively affected radial growth of pitch pine (Pinus rigida Mill.), an intermediate host. There was little or no effect of defoliation on increment of trembling aspen (Populus tremuloides Michx.) and bigtooth aspen (Populus grandidentata Michx.), but both are preferred hosts. Defoliation of host trees in mixed stands resulted in increased increment in the nonhosts tulip-tree (Liriodendron tulipifera L.) and ash (Fraxinus spp.) in the year following defoliation. The effect of defoliation was also evident in the relative production of earlywood and latewood with a pronounced dominance of earlywood production in host trees during the same year as defoliation and often in the following year.


2018 ◽  
Vol 30 (1) ◽  
pp. 233-242
Author(s):  
Chang-Seok Lee ◽  
George R. Robinson ◽  
Ingrid P. Robinson ◽  
Hansol Lee

1991 ◽  
Vol 118 (4) ◽  
pp. 412 ◽  
Author(s):  
Franz K. Seischab ◽  
John M. Bernard
Keyword(s):  
New York ◽  

1995 ◽  
Vol 134 (2) ◽  
pp. 294 ◽  
Author(s):  
John M. Bernard ◽  
Franz K. Seischab

Plant Disease ◽  
1998 ◽  
Vol 82 (8) ◽  
pp. 959-959 ◽  
Author(s):  
Vladimir Vujanovic ◽  
Marc St.-Arnaud ◽  
Peterjürgen Neumann

This is the first report of Naemacyclus fimbriatus (Schwein.) DiCosmo, Peredo & Minter (Rhytismatales) on Pinus rigida, and the first observation of this fungus infecting living needles. N. fimbriatus is known to occur on cone scales of P. brucia, P. halepensis, P. nigra, P. resinosa, and P. sylvestris, as well as fallen needles of P. maritima and P. pinaster, in Europe and North America (1). In September 1997, chlorotic and necrotic second- and third-year needles of pitch pine were observed to have ascomata fruiting bodies that were amphigenous, dark brown to black, immersed to erumpent, circular to subcircular, and 200 to 500 × 150 to 250 μm in size. Asci were club-shaped, eight-spored, and 83 to 98× 8.9 to 9.7 μm. Mature ascospores were phragmo-scolecosporous, 7-septate, and 78 to 91 × 2 to 2.5 μm. From these symptomatic needles, N. fimbriatus was frequently (>70%) isolated on 2% malt agar. In October 1997, fruiting bodies were also observed on dead fallen cones. During the autumn, the fungus produced 1 to 3 brown mycelial cords, 50 to 100 μm in diameter, which grew throughout the litter from the ascomata. The nature of the cords is still unknown. Pitch pine is rare in Québec, and this northernmost population is located about 10 km north of New York State, in the St. Lawrence Valley of Québec. We found that pitch pine was colonized by the fungus in a wide range of edaphic conditions, but more frequently on dry rock outcrops. We believe that unfavorable conditions such as the more than 200 days with frost and thin organic or mineral soil layer may predispose pitch pine to infection by this fungus. Reference: (1) F. Di Cosmo et al. Mycotaxon 21:1, 1984.


2017 ◽  
Vol 53 ◽  
pp. 269-284
Author(s):  
Martin A. Becker ◽  
Rebecca B. Chamberlain ◽  
Harry M. Maisch ◽  
Alex Bartholomew ◽  
John A. Chamberlain

Glacial erratics belonging to the Rickard Hill facies (RHF) of the Saugerties Member of the Schoharie Formation (upper Emsian: Lower Devonian) occur scattered throughout the Piedmont of northern New Jersey and Lower Hudson Valley of New York. These RHF glacial erratics contain an assemblage of trilobites belonging to: Anchiopella anchiops, Burtonops cristatus, Calymene platys, Terataspis grandis, cf. Trypaulites sp. and cf. Coniproetus sp. This RHF glacial erratic trilobite assemblage consists predominately of disarticulated cephala and pygidia that were originally preserved as part of a localized, third-order eustatic sea level lag deposit in the Helderberg Mountains region of central New York State and subsequently transported in glacially plucked blocks by the Hudson-Champlain Lobe of the Laurentide Ice Sheet southward into New Jersey. Physical and chemical weathering during glacial erosion, transportation and deposition of the RHF glacial erratics has revealed some anatomical features of these trilobites in high detail along with other invertebrates. This unique sequence of weathering reveals additional characteristics that bear upon issues of bathymetric controls on upper Schoharie Formation lithology, trilobite faunal abundance and taphonomy during the upper Emsian (Lower Devonian) of eastern New York State.  


2007 ◽  
Vol 24 (1) ◽  
pp. 65-70 ◽  
Author(s):  
Matthew J. Duveneck ◽  
William A. Patterson

Abstract Destructive sampling of 31 pitch pine (Pinus rigida P. Mill) trees ranging in dbh from 2.7 to 42.5 cm and in height from 4.1 to 23.8 m provided a complete inventory of needles and small-diameter branch weights used to characterize canopy fuels to predict fire behavior in pitch pine stands. Regression equations using dbh as an independent variable predict canopy bulk density with an r2 > 0.93. The results provide managers with a method of evaluating the effectiveness of thinning operations in reducing crown fire potential in well-stocked stands. To demonstrate the application of the method, we calculated the wind speed (Crowning Index [CI]) needed to sustain an active crown fire in thinned and unthinned pitch pine stands in Montague, Massachusetts. Thinning to 2.8 m2/ha basal area increased the CI from 34 to 98 km/hour.


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