corals as paleoclimatic archives jens zinke proper june 2004, vu amsterdam
TRANSCRIPT
Environmental tracers in corals
Oxygen isotopes:
- Sea surface temperature- Seawater isotopic composition
Carbon isotopes:
- cloud cover
Sr/Ca, U/Ca, Li/Ca (?):
-Sea surface temperature
U/Ca, Mg/Ca:
-Salinity
U/Th dating of fossil corals
Combined Sr/Ca and d18O:
- Hydrologic balance
14C, Pb-isotopes:
- Ocean circulation- Atmospheric circulation- Upwelling
Ba/Ca, Cd/Ca:
-Terrestrial river runoff- upwelling
Rare Earth Elements (REE):
- biological activity in seawater
Techniques for isotope and trace element ratios:
- Oxygen and carbon isotopes on Mass Spectrometer
- Sr/Ca, Mg/Ca, Ba/Ca on ICP-OES
- U/Ca, Li/Ca, Sr/Ca, Mn/Ca, Ba/Ca on ICP-MS and Laser Ablation ICP-MS
- Sr/Ca, U/Ca, U/Th on TIMS
- Rare Earth Elements with Laser Ablation ICP-MS
- Element mapping and ultra-high-resolution with SIMS and PIXE
Exoskeleton(Aragonite crystals)
Extracellular calcifying fluid
Basal ectodermof coral polyp withsymbiontsfrom seawater
Growth rate effects
slow growth rates (below 3mm/year) = heavy isotopes
McConnaughey, 2003, Coral Reefs 22
Isotopic fractionation
Kinetic fractionation
Non-photosynthetic
photosynthetic
McConnaughey, 2003, Coral Reefs 22
Density banding: first age model
High density = winter
Low density = summer
Major growth axis10-15 m
m
Calibration vs .instrumental data: Linear Regression
Inverse relationship to temperature in isotopes and Sr/Ca ratios !
Combined use of 18O and Sr/Ca: Hydrologic balance
Method in Ren et al., 2002 Geochimica et Cosmochimica Acta 67 (9)
SST / Wind Precip.Evap.
Summer monsoon (July)
Winter monsoon (January) January
July
Coral sites superimposed on SST and monsoonal winds
Western Indian Ocean coral time series
Pfeiffer, 2002; Pfeiffer et al., 2004, Quaternary Research; Zinke et al. (subm)
Changing El Nino frequency derived from a coral 18O record at Kiribati Island (1°N) located within the Nino3 region in the Pacific
Spatial correlation maps coral vs. Global SST:Indian Ocean - ENSO teleconnection: 1970‘s shift?
before 1970 after 1970
Future needs:
- proxies for environmental changes in coastal waters
- process studies of incorporation of proxies into skeleton
- multiple core replication of single core results
- use of more statistical methods to unravel climate information
- net work of coral records for each ocean basin for large scale climate reconstruction
- collaboration with climate modeling community to test future scenarios