Sea urchin development in a global change hotspot, potential for southerly migration of thermotolerant propagules

• Published in: Deep-sea research. Part II, Topical studies in oceanography Topical studies in oceanography, 2011-03, Vol.58 (5), p.712-719
• Main Authors: Byrne, M., Selvakumaraswamy, P., Ho, M.A., Woolsey, E., Nguyen, H.D.
• Format: Article
• Language: English
• Subjects: Climate change; Deep sea; Eastern Australia; Echinoidea; Embryos; Heliocidaris erythrogramma; Larvae; Marine; Migration; Ocean warming; Oceanography; Oceans; Populations; Reduction; Sea urchin larvae; Sea urchins
• ISSN: 0967-0645; 1879-0100
• DOI: 10.1016/j.dsr2.2010.06.010

The distribution of the sea urchin Heliocidaris erythrogramma coincides with the southeast Australia global change hot spot where marine ecosystems are warming significantly due to changes in ocean circulation. To address questions on future vulnerabilities, the thermotolerance of the planktonic life phase of H. erythrogramma was investigated in the climate and regionally relevant setting of projected near-future (2100) ocean warming. Experimental treatments ranged from 18 to 26 °C, with 26 °C representing +3–4 °C above recent ambient sea-surface temperatures. Developmental success across all stages (gastrula, 24 h; larva, 72 h; juvenile, 120 h) decreased with increasing temperature. Development was tolerant to a +1–2 °C increase above ambient, but significant deleterious effects were evident at +3–4 °C. However, larvae that developed through the early bottleneck of normal development at 26 °C metamorphosed successfully. The inverse relationship between temperature and planktonic larval duration (PLD) was seen in a 25% decrease in the PLD of H. erythrogramma at 24 and 26 oC. Ocean warming may be advantageous to a subset of larvae through early settlement and reduction of the vulnerable planktonic period. This positive effect of temperature may help buffer the negative effects of ocean warming. In parallel studies with progeny derived from northern (Coffs Harbour) and southern (Sydney) H. erythrogramma, northern embryos had significantly higher thermotolerance. This provides the possibility that H. erythrogramma populations might keep up with a warming world through poleward migration of thermotolerant propagules, facilitated by the strong southward flow of the East Australian Current. It is uncertain whether H. erythrogramma populations at the northern range of this species, with no source of immigrants, will have the capacity to persist in a warm ocean. Due to its extensive latitudinal distribution, its potential developmental thermotolerance and independence of its lecithotrophic larvae from exogenous food and the need to make a functional skeleton, H. erythrogramma may be particularly robust to ocean change.