@inbook {1420,
	title = {Dynamics of tidal salt barren formation and the record of present-day sea level change},
	booktitle = {The Ecogeomorphology of Tidal Marshes, American Geophysical Union},
	year = {2004},
	note = {id: 1164},
	month = {2004},
	pages = {231-245},
	author = {Hsieh, Y. P.},
	editor = {Fagherazzi, S.}
}
@article {792,
	title = {Soil-productivity relationships and organic matter turnover in dry tropical forests of the Florida Keys},
	journal = {Plant and Soil},
	volume = {253},
	year = {2003},
	note = {702ymTimes Cited:12Cited References Count:46},
	month = {Jun},
	pages = {479-492},
	abstract = {Soils and aboveground production in five types of upland forest in the Florida Keys were examined. Throughout the habitat gradient represented by these forest types, the soils were predominantly shallow and organic, forming in place directly on the limestone bedrock. However, the well-drained soils in the most productive broadleaved forests were deep enough to qualify as Histosols (Folists). Soils decreased in electrical conductivity and increased in nutrient content with increasing aboveground production. At 3-12 Mg ha(-1) yr(-1), production was within the range reported for dry tropical forests. Measured rates of decomposition were moderate or fast, and estimates of the organic C turnover of several soils based on their bomb radiocarbon signature were 100 years or less. In the face of these rapid turnover rates, we attribute the development of organic soils to the absence of mineral residues from weathering of the underlying limestone bedrock. Fast turnover of organic matter, and rapid and efficient cycling of nutrients are necessary to sustain the high production rates obtained on these shallow organic soils.},
	issn = {0032-079x},
	doi = {10.1023/A:1024843130866},
	author = {Ross, M. S. and Coultas, C. L. and Hsieh, Y. P.}
}
@article {930,
	title = {Chemical and carbon isotopic evidence for the source and fate of dissolved organic matter in the northern Everglades},
	journal = {Biogeochemistry},
	volume = {61},
	year = {2002},
	note = {id: 616},
	pages = {269-289},
	doi = {10.1023/A:1020282717732},
	author = {Wang, Y. and Hsieh, Y. P. and Landing, W. M. and Choi, Y. H. and Salters, V. and Campbell, D.}
}
@article {2088,
	title = {Uncertainties and novel prospects in the study of the soil carbon dynamics},
	journal = {Chemosphere},
	volume = {49},
	year = {2002},
	note = {Wang, YangHsieh, Yuch-Ping
eng
England
2002/11/15 04:00
Chemosphere. 2002 Dec;49(8):791-804.
},
	month = {Dec},
	pages = {791-804},
	abstract = {Establishment of the Kyoto Protocol has resulted in an effort to look towards living biomass and soils for carbon sequestration. In order for carbon credits to be meaningful, sustained carbon sequestration for decades or longer is required. It has been speculated that improved land management could result in sequestration of a substantial amount of carbon in soils within several decades and therefore can be an important option in reducing atmospheric CO2 concentration. However, evaluation of soil carbon sources and sinks is difficult because the dynamics of soil carbon storage and release is complex and still not well understood. There has been rapid development of quantitative techniques over the past two decades for measuring the component fluxes of the global carbon cycle and for studying the soil carbon cycle. Most significant development in the soil carbon cycle study is the application of accelerator mass spectrometry (AMS) in radiocarbon measurements. This has made it possible to unravel rates of carbon cycling in soils, by studying natural levels of radiocarbon in soil organic matter and soil CO2. Despite the advances in the study of the soil carbon cycle in the recent decades, tremendous uncertainties exist in the sizes and turnover times of soil carbon pools. The uncertainties result from lack of standard methods and incomplete understanding of soil organic carbon dynamics, compounded by natural variability in soil carbon and carbon isotopic content even within the same ecosystem. Many fundamental questions concerning the dynamics of the soil carbon cycle have yet to be answered. This paper reviews and synthesizes the isotopic approaches to the study of the soil carbon cycle. We will focus on uncertainties and limitations associated with these approaches and point out areas where more research is needed to improve our understanding of this important component of the global carbon cycle.},
	keywords = {Carbon Dioxide/chemistry/metabolism, Carbon Radioisotopes/analysis, Carbon/*chemistry/metabolism, Ecosystem, Kinetics, Models, Chemical, Plants/metabolism, Seasons, Soil/*analysis},
	isbn = {0045-6535 (Print)0045-6535 (Linking)},
	doi = {10.1016/s0045-6535(02)00381-8},
	url = {https://www.ncbi.nlm.nih.gov/pubmed/12430658},
	author = {Wang, Y. and Hsieh, Y. P.}
}
@article {2159,
	title = {Vegetation succession and carbon sequestration in a coastal wetland in northwestern Florida: evidence from carbon isotopes},
	journal = {Global Biogeochemical Cycles},
	volume = {15},
	year = {2001},
	note = {id: 267},
	month = {2001},
	pages = {311-319},
	author = {Choi, Y. and Wang, Y. and Hsieh, Y. P. and Robinson, L.}
}
@conference {1612,
	title = {The distribution and carbon isotopic composition of dissolved organic matter in Florida Everglades (abstract)},
	booktitle = {The Sixth Symposium on Biogeochemistry of Wetlands},
	year = {1999},
	note = {id: 165},
	month = {1999},
	author = {Wang, Y. and Hsieh, Y. P. and Landing, W. M. and Salters, V. and Cooper, W. and Proctor, L.}
}
@article {1485,
	title = {The speciation and sources of dissolved phosphorus in the Everglades (Report)},
	year = {1999},
	note = {id: 1348},
	month = {1999},
	author = {Copper, W. and Hsieh, Y. P. and Landing, W. M. and Proctor, L. and Salters, V. and Wang, Y.}
}
