20th century
; Foraminifera
; Little Ice Age
; Medieval climate anomalies
; Salt-marsh
; Sediments
; Transfer functions
; Uncertainty analysis
; Sea level
; chronology
; foraminifera
; Holocene
; Little Ice Age
; paleoenvironment
; proxy climate record
; reconstruction
; resolution
; saltmarsh
; sea level change
; tide gauge
; transfer function
; New Jersey
; United States
Department of Earth and Ocean Sciences, Tufts University, Medford, MA 02155, United States; Institute of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, United States; Division of Earth Sciences and Earth Observatory of Singapore, Nanyang Technological University, 639798 SG, Singapore; British Geological Survey, Keyworth, Nottingham NG12 5GG, United Kingdom; United States Geological Survey, National Center, Reston, VA 20192, United States; Department of Geological Science, East Carolina University, Greenville, NC 27858, United States; Department of Geosciences, University of Rhode Island, Kingston, RI 02881, United States; School of Forestry and Environmental Studies, Yale University, New Haven, CT 06511, United States; School of Mathematical Sciences (Statistics), Complex Adaptive Systems Laboratory, University College Dublin, Belfield, Dublin 4, Ireland
Recommended Citation:
Kemp A.C.,Horton B.P.,Vane C.H.,et al. Sea-level change during the last 2500 years in New Jersey, USA[J]. Quaternary Science Reviews,2013-01-01,81