Table 1.
Biotic responses to sea surface warming and ocean carbonation/acidification and their feedback potential to the climate system
| Feedback process | Sign of feedback | Sensitivity | Capacity | Longevity |
|---|---|---|---|---|
| Responses to ocean warming | ||||
| Nutrient supply to oligotrophic ocean | +++ | ±0 | ++ | |
| Nutrient supply to HNLC areas | negative | ++ | ++ | +++ |
| Nutrient utilization efficiency | negative | ++ | ++ | +++ |
| Nutrient inventory | positive | ++ | +++ | |
| Organic matter remineralisation | positive | |||
| Responses to ocean acidification | ||||
| Calcification | negative | +† | + | +‡ |
| Ballast effect | positive | +++ | +++ | |
| Stoichiometry | negative | ++† | ++ | ++ |
| Extracellular organic matter production | negative | ++† | +++ | ‡ |
| Nitrogen fixation | negative | ++† | + | ‡ |
Responses are characterized with regard to feedback sign, sensitivity, capacity, and longevity by using best guesses; we use ±0 for negligible, + for low, ++ for moderate, and +++ for high. Empty boxes indicate missing information/ understanding.
†Available information mainly based on short-term perturbation experiments.
‡Potential for adaptation presently unknown. HNLC, high nutrient, low chlorophyll.