Pelagic Food Webs Flashcards
(36 cards)
Classic and microbial food webs linked
Classic and microbial pathways are a useful dichotomy for distinguishing the several fates of C PP in marine ecosystems
Recent evidence shows that the microbial food web is a fundamental and almost permanent feature of oligotrophic and eutrophic coastal upwelling areas.
Biological Carbon Pump zoop contributions
Sloppy feeding
- excretion
- egestion
- mucous production
- exudates, reproduction
- migration
- death
How to quantify C or energy flowing through webs
Bioenergetics, how much energy to metabolism, growth, reproduction
Fatty acid stable isotope analysis, life history info
Measuring primary and secondary production
Ecosystem based modelling
Bioenergetic approach
New growth/production (G) = ingestion (R) - Faeces (E) - Excretion (U) - Respiration (T)
or
Net growth/production = assimilated food (AR) - respiration (T)
Growth Yield
Ygr = growth/growth + respiration or
Ygr = growth/food intakea
= 10-30%
Growth yield depends on
Type of organism
Level of complexity
Swimming ability
Stage of life
Trophic yield
Ty = production at trophic level (t+1) / production at trophic level (t)
Total efficiency (Ty)n
Trophic yield = ecological transfer efficiency (10-30%)
Trophic Energy Pyramid
Amount of biomass decreases as you move up the trophic levels because only ~10% energy within a trophic level is available for the next trophic level
the amount of PP at the base drives trophic structure
Match-mismatch, temporal
In a mismatch there aren’t enough zooplankton to feed all recruits so can’t develop
Match-mismatch, spatially
Warm climate conditions reduced spatial overlap, results in lower overwinter survival and recruitment success of juveniles to age 1
Colder climate conditions increased spatial overlap results in higher growth, overwinter survival and recruitment success of juvenile fish to age 1.
Up welling ecosystems
Eastern boundary upwelling systems (EBUS) cover <1% of the ocean surface but provide up to 20% of the world’s capture fisheries due to their high levels of production fuelled by nutrient-rich, cold deep water.
EBUS, oceanography
Wind blowing pushes warm surface water away from the coast
Displaced water replaced by deep, cold, nutrient rich water rising to the surface.
Nutrient rich water fertilizes surface waters, high PP
EBUS ecology
short efficient food chains, lots of fish
EBUS, normal climate
Normal:
- Low pressure W Pacific and high pressure E pacific cause trade winds to move surface water to west, upwelling and shallow thermocline
EBUS, El Nino
High pressure system weakens, trade winds reduce
Warm surface water flows easy, deepens thermocline and prevents upwelling.
EBUS, la nina
Unusually strong trade winds bringing deep cold water to the surface resulting in colder water than usual
EBUS, effects of upwelling intensity
Normal, zoop pop grow and control phyto, conventional marine food web
Intense upwelling exports zoop quicker than pop growth.
Strong swimming sardines able to remain and consume phyto, local food web collapse and free nutrients flow off shore
Intense upwelling exports zoop too rapidly, phyto not grazed so die and decay, noxious gas, unused zoop offshore fed on by jelly blooms
Cali Food Web
Euphasiids are the most important for energy transfer pathway
Large production of the lower trophic production eaten (green) is transferred to the higher trophic levels (red)
Californa current system food web model
Jellyfish act as a production loss pathway
Little of the production consumed was passed upward, jellies arent consumed
If jelly consumption reduced by 20%, productivity increases to upper trophic levels
Cali El Nino effect
Deep thermocline
more complex food web
Reduced nutrients and populations
Benguela upwelling system
Sardines, anchovies, mackerel and hake fluctuated since the 50s.
Alternation between planktivory and predatory fish
10-fold increase in copepod biomass since 50s
Collapse of sardine fishery
Sardines replaced by mackerel and goby
Benguela jellification
Overfishing of small pelagic fish triggered chain of events resulting in rise of jellyfish and the bearded goby
energy flow is diverted away from the higher trophic level (HTL) production towards benthos and detritus
Oligotrophic subtropical gyres
Once thought of as deserts, low nutrient inputs and productivity
Subtropical gyres are much more dynamic systems
Nutrients and Chl a
Surface nitrate (low f ratio) with clearly defined vertical structure and the DCM
0.05-0.1mg Chl a/m3