Relation of plant species to substrate, landscape position, and aspect in north central Massachusetts

1991 ◽  
Vol 21 (8) ◽  
pp. 1245-1252 ◽  
Author(s):  
Gordon G. Whitney

Vegetation–site relationships in the region about the Harvard Forest in north central Massachusetts were explored by means of contingency table and cluster analyses of presence–absence data. Most of the arboreal species, the shrubs, and the ferns were strongly associated with segments of a microclimate – soil moisture gradient determined by landscape position and substrate. Cluster analysis of the species suggested the existence of a fertility gradient, with the more nutrient demanding white ash (Fraxinusamericana L.), sugar maple (Acersaccharum L.) and basswood (Tiliaamericana L.) on one end of the gradient and pitch pine (Pinusrigida Mill.), scrub oak (Quercusilicifolia Wangenh.), and aspen (Populus sp.) on the more impoverished sites. An analysis of the feasibility of determining vegetation–site relationships in an area with a long history of human disturbances concludes the report.

1990 ◽  
Vol 20 (9) ◽  
pp. 1479-1484 ◽  
Author(s):  
F. A. Bazzaz ◽  
J. S. Coleman ◽  
S. R. Morse

We examined how elevated CO2 affected the growth of seven co-occurring tree species: American beech (Fagusgrandifolia Ehrh.), paper birch (Betulapapyrifera Marsh.), black cherry (Prunusserotina Ehrh.), white pine (Pinusstrobus L.), red maple (Acerrubrum L.), sugar maple (Acersaccharum Marsh.), and eastern hemlock (Tsugacanadensis (L.) Carr). We also tested whether the degree of shade tolerance of species and the age of seedlings affected plant responses to enhanced CO2 levels. Seedlings that were at least 1 year old, for all species except beech, were removed while dormant from Harvard Forest, Petersham, Massachusetts. Seeds of red maple and paper birch were obtained from parent trees at Harvard Forest, and seeds of American beech were obtained from a population of beeches in Nova Scotia. Seedlings and transplants were grown in one of four plant growth chambers for 60 d (beech, paper birch, red maple, black cherry) or 100 d (white pine, hemlock, sugar maple) under CO2 levels of 400 or 700 μL•L−1. Plants were then harvested for biomass and growth determinations. The results showed that the biomass of beech, paper birch, black cherry, sugar maple, and hemlock significantly increased in elevated CO2, but the biomass of red maple and white pine only marginally increased in these conditions. Furthermore, there were large differences in the magnitude of growth enhancement by increased levels of CO2 between species, so it seems reasonable to predict that one consequence of rising levels of CO2 may be to increase the competitive ability of some species relative to others. Additionally, the three species exhibiting the largest increase in growth with increased CO2 concentrations were the shade-tolerant species (i.e., beech, sugar maple, and hemlock). Thus, elevated CO2 levels may enhance the growth of relatively shade-tolerant forest trees to a greater extent than growth of shade-intolerant trees, at least under the light and nutrient conditions of this experiment. We found no evidence to suggest that the age of tree seedlings greatly affected their response to elevated CO2 concentrations.


1942 ◽  
Vol 12 (1/2) ◽  
pp. 100
Author(s):  
E. G. R. Taylor ◽  
Hugh M. Raup ◽  
Reynold E. Carlson
Keyword(s):  
Land Use ◽  

Paleobiology ◽  
10.1666/12030 ◽  
2013 ◽  
Vol 39 (2) ◽  
pp. 235-252 ◽  
Author(s):  
Cindy V. Looy

Within conifers, active abscission of complete penultimate branch systems is not common and has been described mainly from juveniles. Here I present evidence for the abscission of penultimate branch systems within early so-called walchian conifers—trees with a plagiotropic branching pattern. The specimens studied originate from a middle Early Permian gymnosperm-dominated flora within the middle Clear Fork Group of north-central Texas. Complete branch systems of three walchian conifer morphotypes are preserved; all have pronounced swellings and smooth separation faces at their bases. The source plants grew in a streamside habitat under seasonally dry climatic conditions. The evolution of active branch abscission appears to correspond to an increase in the size of conifers, and this combination potentially contributed to the restructuring of conifer-rich late Paleozoic landscapes. Moreover, trees shedding branch systems and producing abundant litter have the potential to affect the fire regime, which is a factor of evolutionary importance because wildfires must have been a source of frequent biotic disturbance throughout the hyperoxic Early Permian.


2009 ◽  
Vol 10 (1) ◽  
pp. 8 ◽  
Author(s):  
Alison E. Robertson ◽  
Silvia R. Cianzio ◽  
Sarah M. Cerra ◽  
Richard O. Pope

Phytophthora root and stem rot (PRR), caused by the oomycete Phytophthora sojae, is an economically important soybean disease in the north central region of the United States, including Iowa. Previous surveys of the pathogenic diversity of P. sojae in Iowa did not investigate whether multiple pathotypes of the pathogen existed in individual fields. Considering the many pathotypes of P. sojae that have been reported in Iowa, we hypothesized multiple pathotypes could exist within single fields. In the research reported herein, several soil samples were collected systematically from each of two commercial fields with a history of PRR in Iowa, and each soil sample was baited separately for isolates of P. sojae. Numerous pathotypes of P. sojae were detected from both fields. As many as four pathotypes were detected in some soil samples (each consisting of six to eight soil cores), which suggests that a single soybean plant could be subjected to infection by more than one pathotype. This possibility presents important implications in breeding resistant cultivars and in the management of PRR. Accepted for publication 14 July 2009. Published 8 September 2009.


2018 ◽  
Vol 50 ◽  
pp. 91-97 ◽  
Author(s):  
Quan Zhou ◽  
Hang Shi ◽  
Chengpo Liu ◽  
Kerong Zhang ◽  
Quanfa Zhang ◽  
...  

1968 ◽  
Vol 44 (6) ◽  
pp. 31-35 ◽  
Author(s):  
Carl H. Winget

Second-growth, tolerant hardwood stands developed rapidly and, almost entirely from shade-tolerant advance growth, regardless of cutting intensity. Non-commercial woody species were seldom important competitors. Sugar maple, associated with beech on upland and balsam fir on lowland sites, was the dominant species. Yellow birch, basswood and hemlock, important contributors to wood volumes harvested, were minor components of second-growth stands. Valuable minor species such as red oak, white ash, and black cherry had practically disappeared. The application of known techniques for regenerating disturbance-dependent species is urgently required.


1986 ◽  
Vol 3 (2) ◽  
pp. 69-72 ◽  
Author(s):  
Susan Laurane Stout

Abstract Planting of northern hardwood species interests forest landowners and managers who wish to continue growing pure or nearly pure stands of high-value species, enhance old-field conversion to preferred species, or reforest areas where natural regeneration has failed. Little data on planted hardwoods can be found, however. This paper reports on 22 years of growth of a northern hardwood plantation established in 1961 containing red maple, black cherry, sugar maple, and white ash. The data show that plantings of these species can succeed on good sites with weed control over the first few years, protection from animal predators, and close initial spacing. North. J. Appl. For. 3:69-72, June 1986.


2019 ◽  
Vol 44 (5) ◽  
pp. 605-623
Author(s):  
Zhixin Hao ◽  
Jingyun Zheng ◽  
Yingzhuo Yu ◽  
Danyang Xiong ◽  
Yang Liu ◽  
...  

The Ancient Silk Road has a history of more than 2000 years and gave birth to the diversities of culture between East and West. Climate change may have played a crucial role in this process and in the flourishing and decline of civilizations. In this work, high-resolution temperature reconstructions covering more than 1000 years along the Ancient Silk Road are reviewed, and the main characteristics of temperature and hydroclimatic changes are summarized. Four warm stages occurred that included the 1st–3rd centuries, the late 7th century to the early 11th century, the mid-12th century to the mid-13th century, and since the 20th century, and three cold stages, including the 4th century to the early 7th century, the middle of the 11th century to the early 12th century, and the end of the 13th century to the mid-19th century, occurred. Within these various stages, regional differences existed in amplitudes and starting–ending years of the cold/warm phases. Wetness and dryness variabilities during the Medieval Climate Anomaly (MCA) were greater than during the Little Ice Age in Northwestern China. The climate was dry during the MCA in Central Asia, South Scandinavia, and North-central Europe. In addition, the climate backgrounds of several famous kingdoms flowering and social events that flourished during these times, such as the Roman Empire, the Loulan Kingdom, the Tibetan Kingdom, and the three unprecedented Mongol westward conquests, are discussed.


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