The Central Indo-Pacific (or CIP if you're stuck for time) is a highly diverse region of the ocean. But how did it get to be this way? It's this question which is the topic for today's episode.

Sources for this episode:

Ivany, L. C., Patterson, W. P. and Lohmann, K. C. (2000), Cooler winters as a possible cause of mass extinctions at the Eocene/Oligocene boundary. Nature 407: 887- 890.
Jones, K. R., Klein, C. J., Halpern, B. S., Venter, O., Grantham, H., Kuempel, C. D., Shumway, N., Friedlander, A. M., Possingham, H. P. and Watson, J. E. M. (2018), The Location and Protection Status of Earth’s Diminishing Marine Wilderness. Current Biology 28: 2506- 2512.
Miller, E.C., Hayashi, K. T., Song, D., Wiens, J. J., (2018) Explaining the ocean’s richest biodiversity hotspot and global patterns of fish diversity. Proceedings of the Royal Society B 285: 20181314.
Renema, W., Bellwood, D. R., Braga, J. C., Bromfield, K., Hall, R., Johnson, K. G., Lunt, P., Meyer, C. P., McMonagle, L. B., Morley, R. J., O'Dea, A., Todd, J. A., Wesselingh, F. P., Wilson, M. E. J. and Pandolfi, J. M. (2008), Hopping Hotspots: Global Shifts in Marine Biodiversity. Science (321): 654- 657.
Siqueira, A. C., Bellwood, D. R. and Cowman, P. F. (2019), Historical biogeography of herbivorous coral reef fishes: The formation of an Atlantic fauna. Journal of Biogeography.
Author unknown, Wikipedia (date unknown), Coral (online) [Accessed 17/01/2021].
Author unknown, Wikipedia (date unknown), Eocene (online) [Accessed 17/01/2021].

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