MONITORING FOREST SOILS OVER TIME TO UNDERSTAND ACIDIC DEPOSITION EFFECTS AND RECOVERY

2018 ◽  
Author(s):  
Gregory B. Lawrence ◽  
◽  
Paul W. Hazlett ◽  
Ivan J. Fernandez ◽  
Rock Ouimet ◽  
...  
Author(s):  
Dan Binkley ◽  
Charles T. Driscoll ◽  
H. Lee Allen ◽  
Philip Schoeneberger ◽  
Drew McAvoy

Author(s):  
Dan Binkley ◽  
Charles T. Driscoll ◽  
H. Lee Allen ◽  
Philip Schoeneberger ◽  
Drew McAvoy

mSphere ◽  
2018 ◽  
Vol 3 (3) ◽  
Author(s):  
James B. Anderson ◽  
Dahlia Kasimer ◽  
Wenjing Xia ◽  
Nicolas C. H. Schröder ◽  
Patrick Cichowicz ◽  
...  

ABSTRACT One might expect yeasts in soil to be highly dispersed via water or insects, forming ephemeral, genetically heterogeneous populations subject to competition and environmental stochasticity. Here, we report persistence of genotypes of the yeast Saccharomyces paradoxus in space and time. Within 1 km 2 in a mixed hardwood forest on scales from centimeters to tens of meters, we detected persistence over 3 years of native genotypes, identified by single nucleotide polymorphisms (SNPs) genome-wide, of the wild yeast Saccharomyces paradoxus growing around Quercus rubra and Quercus alba . Yeasts were recovered by enrichment in ethanol-containing medium, which measures only presence or absence, not abundance. Additional transplantation experiments employed strains marked with spontaneous defects in the URA3 gene, which also confer resistance to 5-fluoroorotic acid (5FOA). Plating soil suspensions from transplant sites on 5FOA-containing medium permitted one-step quantification of yeast CFU, with no interference from other unmarked yeasts or microorganisms. After an initial steep decrease in abundance, the yeast densities fluctuated over time, increasing in association with rainfall and decreasing in association with drought. After 18 months, the transplanted yeasts remained in place on the nine sites. In vitro transplantation experiments into nonsterile soil in petri dishes showed similar patterns of persistence and response to moisture and drought. To determine whether Saccharomyces cerevisiae , not previously recovered from soils regionally, can persist in our cold climate sites, we transplanted marked S. cerevisiae alone and in mixture with S. paradoxus in the fall of 2017. Five months later, S. cerevisiae persisted to the same extent as S. paradoxus . IMPORTANCE Saccharomyces yeasts are intensively studied in biological research and in their domesticated roles in brewing and baking, and yet, remarkably little is known about their mode of life in forest soils. We report here that resident genotypes of the yeast S. paradoxus are persistent on a time scale of years in their microhabitats in forest soils. We also show that resident genotypes can be replaced by transplanted yeast genotypes. The high inoculum levels in experimental transplantations rapidly decreased over time, but the transplanted genotypes persisted at low abundance. We conclude that, in forest soils, Saccharomyces yeasts exist at very low abundance and that dispersal events are rare.


1986 ◽  
Vol 33 (2-4) ◽  
pp. 231-253 ◽  
Author(s):  
Pekka Kauppi ◽  
Juha Kämäri ◽  
Maximilian Posch ◽  
Lea Kauppi ◽  
Egbert Matzner

2005 ◽  
Vol 35 (5) ◽  
pp. 1109-1121 ◽  
Author(s):  
T G Huntington

Forest harvesting and acidic deposition can cause substantial decreases in the calcium (Ca) inventory of forest soils if such losses are not replenished through mineral weathering, atmospheric deposition, or fertilization. The net balance between losses and gains defines the forest Ca status. Site-specific studies have measured Ca pools and fluxes in Maine forests, but no synthesis has been published. In this paper, I review the literature on forest Ca and assess the current status and potential future trends. Forest soils in Maine are currently at lesser risk of Ca depletion compared with many forest soils in the central and southeastern United States, because levels of acidic deposition and rates of Ca accumulation in trees are lower in Maine. The rate of Ca accumulation in trees is reduced in Maine as a result of lower growth rates and a higher proportion of conifer trees that require less Ca than hardwoods. However, field-scale biogeochemical studies in Maine and New Hampshire, and regional estimates of harvest removals and soil inventories coupled with low weathering estimates, indicate that Ca depletion is a realistic concern in Maine. The synthesis of site-specific and regional data for Maine in conjunction with the depletion measured directly in surrounding areas indicates that the Ca status of many forest soils in Maine is likely declining. Ca status could decrease further in the future if forest growth rates increase in response to climate trends and recovery from insect-induced mortality and excessive harvesting in recent years. Proposed climate change induced reductions in spruce and fir and increases in hardwoods would also increase the risk of Ca depletion.


1987 ◽  
Vol 51 (2) ◽  
pp. 446 ◽  
Author(s):  
P. K. Khanna ◽  
J. Prenzel ◽  
K. J. Meiwes ◽  
B. Ulrich ◽  
E. Matzner

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