Simulation of the Potential Impacts of Acidic Deposition on Forest Soils in the South

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

2022 ◽  
Author(s):  
Paulo Saraiva Camara ◽  
Fabio Bones ◽  
Fabyano Lopes ◽  
Fabio Oliveira ◽  
Cristine Barreto ◽  
...  

Abstract Located 1,140 km from the South American coastline in the South Atlantic Ocean, and with an age of 4 million years, Trindade Island is the most recent volcanic component of Brazilian territory. Its vegetation was severely damaged by human influence in particular through the introduction of exotic grazing animals such as goats. However, since the complete eradication of goats and other feral animals in the late 1990s, the island’s vegetation has been recovering and even some endemic species that had been considered extinct have been rediscovered. In this study we set out to characterize the contemporary microbial diversity of Trindade Island forest soils using metabarcoding by High Throughput Sequencing (HTS). Sequences of representative of two domains (Bacteria and Archaea) and five kingdoms (Fungi, Metazoa, Protozoa, Chromista and Viridiplantae) were identified. Bacteria were represented by 20 phyla and 116 taxa, while and Archaea by only one taxon. Fungi were represented by seven phyla and 250 taxa, Viridiplantae by five phyla and six taxa, Protozoa by five phyla and six taxa, Metazoa by three phyla and four taxa and Chromista by two phyla and two taxa. Even after the considerable anthropogenic impacts and devastation of the island’s natural forest, our sequence data revealed the presence of a rich, diverse and complex diversity of microorganisms, invertebrates and plants.


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.


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