Zobrazeno 1 - 10
of 42
pro vyhledávání: '"David J Velinsky"'
Publikováno v:
PLoS ONE, Vol 8, Iss 5, p e62891 (2013)
Habitat degradation and species introductions are two of the leading causes of species declines on a global scale. Invasive species negatively impact native species through predation and competition for limited resources. The impacts of invasive spec
Externí odkaz:
https://doaj.org/article/ae3d39ac86c547e4bcae167fc73a175b
Autor:
Elizabeth Burke Watson, Kaitlin Tucker, Kari St. Laurent, Lena Champlin, Christopher K. Sommerfield, David J. Velinsky
Publikováno v:
Data, Vol 5, Iss 1, p 11 (2020)
Quantifying carbon sequestration by tidal wetlands is important for the management of carbon stocks as part of climate change mitigation. This data publication includes a spatial analysis of carbon accumulation rates in Barnegat and Delaware Bay tida
Publikováno v:
Journal of Coastal Research. 78:60-69
Paudel, B.; Weston, N.; O'Connor, J.; Sutter, L., and Velinsky, D., 2017. Phosphorus dynamics in the water column and sediments of Barnegat Bay, New Jersey. In: Buchanan, G.A.; Belton, T.J., and Paudel, B. (eds.), A Comprehensive Assessment of Barneg
Publikováno v:
Journal of Coastal Research. 78:70-78
Velinsky, D.J.; Paudel, B.; Quirk, T.; Piehler, M., and Smyth, A., 2017. Salt marsh denitrification provides a significant nitrogen sink in Barnegat Bay, New Jersey. In: Buchanan, G.A.; Belton, T.J., and Paudel, B. (eds.), A Comprehensive Assessment
Publikováno v:
Journal of Coastal Research. 78:79-88
Velinsky, D.J.; Paudel, B.; Belton, T.J., and Sommerfield, C.K., 2017. Tidal marsh record of nutrient loadings in Barnegat Bay, New Jersey. In: Buchanan, G.A.; Belton, T.J., and Paudel, B. (eds.), A Comprehensive Assessment of Barnegat Bay-Little Egg
Publikováno v:
Estuarine, Coastal and Shelf Science. 182:179-189
Organic carbon sequestration in salt marsh soils is a function of factors that influence both spatial variability and chemical stability of accumulating carbon. Refractory carbon (slowly decomposed) may be the most important in terms of long-term seq
Publikováno v:
Ecological Informatics. 34:1-12
Environmental variables such as river inflow, dissolved chemicals, temperature, total suspended solids, dissolved oxygen, and pH are the environmental drivers that maintain phytoplankton growth in estuaries. Spatial variability of environmental drive
Autor:
Stephen Crooks, Christopher K. Sommerfield, Timothy M. Shaw, Lauren Brown, Kevin D. Kroeger, William R. Reay, Joseph M. Smoak, Judith Z. Drexler, Norman B. Bliss, James R. Holmquist, Brandon M. Boyd, Meagan Eagle Gonneea, Joshua L. Breithaupt, Elizabeth Burke Watson, Tiffany G. Troxler, Isa Woo, Benjamin P. Horton, Mark S. Woodrey, Kevin J. Buffington, Ryan P. Moyer, David J. Velinsky, Lyndie A. Hice, Donald E. Weller, Nicole Dix, James T. Morris, Karen M. Thorne, Lisamarie Windham-Myers, Matthew C. Ferner, John C. Callaway, Kristin Wilson Grimes, J. Patrick Megonigal, Lisa Schile-Beers, Erik M. Smith, Glen M. MacDonald
Publikováno v:
Scientific reports, vol 8, iss 1
Scientific Reports
Scientific Reports, Vol 8, Iss 1, Pp 1-16 (2018)
Scientific Reports
Scientific Reports, Vol 8, Iss 1, Pp 1-16 (2018)
Tidal wetlands produce long-term soil organic carbon (C) stocks. Thus for carbon accounting purposes, we need accurate and precise information on the magnitude and spatial distribution of those stocks. We assembled and analyzed an unprecedented soil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b0fb308f3a9c83f43cbb9ff4f90d3f3
https://escholarship.org/uc/item/1sk7k1j2
https://escholarship.org/uc/item/1sk7k1j2
2013 Benjamin Franklin Medal in Earth and Environmental Science presented to Robert Arbuckle Berner†
Publikováno v:
Journal of the Franklin Institute. 352:2591-2595
The processes and cycles of the Earth that arise through the interactions of its biota, its soil and rocks, its atmosphere and oceans, are intricate and complex. These cycles also provide and define the environment that makes all life on Earth possib
Publikováno v:
Journal of Paleolimnology. 53:107-121
The chronology of a 184-cm-long sediment core from Onondaga Lake, New York (USA), is known with annual certainty from 2006 to the 1880s. Sediment age is known with similar precision, but less confidence, from the 1880s to the 1820s. Paired dark and l