Publications

C. Ainsworth (2008) Ferryboxes Begin to Make Waves. NewsFocus Item, Science, 322: 1627-1629.

H. S. Findlay, T. Tyrrell, R. G. J. Bellerby, A. Merico, and I. Skjelvan (2008) Carbon and nutrient mixed layer dynamics in the Norwegian Sea. Biogeosciences, 5, 1395-1410.

Zeebe RE, Zachos JC, Caldeira K, Tyrrell T. (2008) Carbon emissions and acidification. Science, 321: 51-52.

Merico A, Tyrrell T, PA Wilson. (2008) Eocene/Oligocene ocean de-acidification linked to Antarctic glaciation by sea-level fall, Nature, 452: 979-983.

MD Iglesias-Rodriguez, P Halloran, REM Rickaby, E Colmenero-Hidalgo, JR Gittins, DRH Green, T Tyrrell, SJ Gibbs, P von Dassow, E Rehm, EV Armbrust and IR Hall. (2008) Phytoplankton calcification in a high CO2 world, Science, 320: 336-340.

T. Tyrrell, B. Schneider, A. Charalampopoulou, and U. Riebesell. (2008) Coccolithophores and calcite saturation state in the Baltic and Black Seas. Biogeosciences,  5: 485-494.

Tyrrell T. (2008) Calcium carbonate cycling in future oceans and its influence on future climates. Contribution to Memorial Volume (Festschrift) for Patrick Holligan. Journal of Plankton Research, 30(2): 141-156.

Tyrrell T, Shepherd JG, Castle S. (2007) The long-term legacy of fossil fuels. Tellus B, 59: 664-672.

Gibbs, S. J., Bralower, T. J., Bown, P. R., Zachos, J. & Bybell, L. (2006). Shelf and open-ocean calcareous phytoplankton assemblages across the Paleocene-Eocene Thermal Maximum: Implications for global productivity gradients. Geology 34, 233-236.

Gibbs, S. J., Bown, P. R., Sessa, J., Bralower, T. J., and Wilson, P. A. (2006). Nannoplankton extinction and origination rates across the Paleocene-Eocene Thermal Maximum. Science 314, 1770-1773.

Merico A, Tyrrell T, Cokacar T. (2006) Is there any relationship between phytoplankton seasonal dynamics and the carbonate system? Journal of Marine Systems, 59: 120-142.

Tyrrell T, Zeebe RE. (2004) Increasing carbonate ion concentration during the last 100 million years. Geochimica et Cosmochimica Acta, 68(17): 3521-3530.