Intensification of the meridional temperature gradient in the Great barrier reef following the last glacial maximum

Thomas Felis, Helen V. McGregor, Braddock K. Linsley, Alexander W. Tudhope, Michael K. Gagan, Atsushi Suzuki, Mayuri Takeuchi, Alexander L. Thomas, Tezer M. Esat, William G. Thompson, Manish Tiwari, Donald C. Potts, Manfred Mudelsee, Yusuke Yokoyama, Jody M. Webster

Research output: Contribution to journalArticle

31 Citations (Scopus)

Abstract

Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and δ 18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.

Original languageEnglish
Article number4102
JournalNature Communications
Volume5
DOIs
Publication statusPublished - Jun 17 2014
Externally publishedYes

Fingerprint

reefs
Reefs
Thermal gradients
temperature gradients
sea surface temperature
Temperature
Oceans and Seas
Anthozoa
coolers
drying
temperature
Drying
expansion
Water
water
Growth

ASJC Scopus subject areas

  • Biochemistry, Genetics and Molecular Biology(all)
  • Chemistry(all)
  • Physics and Astronomy(all)

Cite this

Felis, T., McGregor, H. V., Linsley, B. K., Tudhope, A. W., Gagan, M. K., Suzuki, A., ... Webster, J. M. (2014). Intensification of the meridional temperature gradient in the Great barrier reef following the last glacial maximum. Nature Communications, 5, [4102]. https://doi.org/10.1038/ncomms5102

Intensification of the meridional temperature gradient in the Great barrier reef following the last glacial maximum. / Felis, Thomas; McGregor, Helen V.; Linsley, Braddock K.; Tudhope, Alexander W.; Gagan, Michael K.; Suzuki, Atsushi; Takeuchi, Mayuri; Thomas, Alexander L.; Esat, Tezer M.; Thompson, William G.; Tiwari, Manish; Potts, Donald C.; Mudelsee, Manfred; Yokoyama, Yusuke; Webster, Jody M.

In: Nature Communications, Vol. 5, 4102, 17.06.2014.

Research output: Contribution to journalArticle

Felis, T, McGregor, HV, Linsley, BK, Tudhope, AW, Gagan, MK, Suzuki, A, Takeuchi, M, Thomas, AL, Esat, TM, Thompson, WG, Tiwari, M, Potts, DC, Mudelsee, M, Yokoyama, Y & Webster, JM 2014, 'Intensification of the meridional temperature gradient in the Great barrier reef following the last glacial maximum', Nature Communications, vol. 5, 4102. https://doi.org/10.1038/ncomms5102
Felis, Thomas ; McGregor, Helen V. ; Linsley, Braddock K. ; Tudhope, Alexander W. ; Gagan, Michael K. ; Suzuki, Atsushi ; Takeuchi, Mayuri ; Thomas, Alexander L. ; Esat, Tezer M. ; Thompson, William G. ; Tiwari, Manish ; Potts, Donald C. ; Mudelsee, Manfred ; Yokoyama, Yusuke ; Webster, Jody M. / Intensification of the meridional temperature gradient in the Great barrier reef following the last glacial maximum. In: Nature Communications. 2014 ; Vol. 5.
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