Lecture 13 Flashcards
Speed of ocean temperature rises
Rising by 0.1 degree Celsius per decade (1960-2009)
Predictions of changes due to ocean temperature increase by 2100
Mora et al. 2013
Ocean surface temperature increased by 2-3 degrees Celsius
pH decline by 0.2 units
Oxygen concentration decrease by 2-4 units
Ocean productivity could decrease by 2% to 20%
Will affect all marine habitats
Effects greatest in surface waters and shallow habitats
When is the real change in marine habitats expected to come?
2030
Marine habitats will enter new climate regime before terrestrial climate
Poorer countries will enter first
Potential impacts in marine life: organismal level
change in body size, reproduction, primary productivity, habitats
Potential impacts in marine life: population level
Changes in population growth, abundance, species distribution
Potential impacts in marine life: community/ecosystem level
Changes in community structure, trophic interaction, biodiversity
Potential impacts in marine life: fisheries/economics
Changes in fisheries catch, economics of fishing, fishery management
Potential impacts in marine life: global issues
Human population growth, migration, development, food supply and energy prices
Biogeographic shifts due to climate warming
Most species studied show poleward latitudinal shifts
However, some species show lower poleward distribution shifts than expected - they may be constrained by ‘essential’ habitat
Heatwave in south east Indian ocean
2011
Wernberg et al. 2013
Caused massive shifts in abundance of local species
Evidence of results of marine heatwaves increasing in frequency
Smale et al. (2019)
More and more coral bleaching
Decrease in seagrass density
Giant kelp biomass changes
What causes “tropicalisation” of fisheries?
Poleward shifts and local abundance changes
Mean temperature of catch is increasing
(MTC = average inferred temperature preference of exploited species weighted by their annual catch)
Temperature and body size
Increased temperatures lead to greater metabolic costs
As environmental temperature increases from lower critical temperature, there is a linear increase in growth until pejus temperature is reached, after which growth rate declines rapidly and ceases at the upper critical temperatures
Smaller body sizes are therefore expected at high temperatures
What is phenology?
The study of the timing of life history events
Climate change and phenology
- Climate determines the timing of seasonal marine events
- Warmer temperatures may shift life history events to occur earlier
- E.g. NE Atlantic zooplankton blooms produced earlier in warmer waters