Home

About

Advanced Search

Browse by Discipline

Scientific Societies

E-print Alerts

Add E-prints

E-print Network
FAQHELPSITE MAPCONTACT US


  Advanced Search  

 
Deep-sea coral aragonite as a recorder for the neodymium isotopic composition of seawater
 

Summary: Deep-sea coral aragonite as a recorder for the neodymium
isotopic composition of seawater
Tina van de Flierdt a,b,
, Laura F. Robinson c
, Jess F. Adkins d
a
Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, Exhibition Road, London SW7 2AZ, UK
b
Lamont-Doherty Earth Observatory and Department of Earth and Environmental Sciences, Columbia University, 61 Route 9W,
Palisades, NY 10964, USA
c
Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
d
California Institute of Technology, MS100-23, 1200 E. California Boulevard, Pasadena, CA 91125, USA
Received 15 March 2010; accepted in revised form 27 July 2010; available online 6 August 2010
Abstract
Deep-sea corals have been shown to be useful archives of rapid changes in ocean chemistry during the last glacial cycle.
Their aragonitic skeleton can be absolutely dated by UTh data, freeing radiocarbon to be used as a water-mass proxy. For
certain species of deep-sea corals, the growth rate allows time resolution that is comparable to ice cores. An additional proxy
is needed to exploit this opportunity and turn radiocarbon data into rates of ocean overturning in the past.

  

Source: Adkins, Jess F. - Division of Geological and Planetary Sciences, California Institute of Technology

 

Collections: Environmental Sciences and Ecology; Geosciences