// lecture 29 Flashcards
coral health is highly dependent on
phytoplankton algae that provides nutrients for slow growing coral. algae are expelled by coral when the temp. gets too warm (24 C), so color of reef reflects color of underlying (dead) coral (white).
coral polyps
living creatures, calcite substrate is their home.
coral symbiosis
- partnership goes back to the Triassic 210 Mya.
- corals lived in relatively nutrient-free regions, not unlike today’s subtropical regions.
- dinoflagellates (algae) live inside the coral’s tissues.
- the algae perform photosynthesis to produce nutrients.
- the coral in turn emits waste products in the form of ammonium, which the algae consume.
- this prevents vital nutrients from drifting away in the current and allow both species to thrive in nutrient-poor water. coral really took off with symbiosis.
- symbiotic corals outperform non-symbiotic corals 10-1.
dinoflagellates (brown algae)
can swim free with their tail. when they incorporate into coral, they lose their tail. they can be ejected into the water by the coral if stressed. this causes the coral to turn white and begin to starve. if good conditions return soon enough, the dinoflagellates can return to the coral, if not the coral polyps die.
symbiodinium reach
high cell densities through prolific mitotic division in the endodermal tissues of many shallow tropical and sub-tropical cnidarians.
coral bleaches in
el nino years and with global warming.
1997-1998 El Nino and coral
16% of all coral were damaged. Some bounced back. corals could become rare on tropical and subtropical reefs by 2050 due to the combined effects of increasing CO2 and increasing frequency of bleaching events.
by 2030 or 2050, bleaching thresholds will be
exceeded annually or bi-annually at the majority of reefs worldwide.
value of coral reefs in the US
NOAA estimates the commercial value of US fisheries from coral reefs is over $100 million. revenues from diving tours, etc. based near reef ecosystems are in the billions. sources of medicine.
more possible ocean changes due to temp.
- increased disease in fish
- poleward movement of some species (tuna, marlin, cod)
- increased mortality of winter flounder eggs and larvae
- marine mammals, birds, seals, sea lions, and walruses feed mainly on plankton, fish, & squid and are vulnerable to changes in prey in response to climatic factors.
- nesting of sea turtles is strongly affected by temp.
the blob
unusually warm SST off the North American west coast in 2013-2014.
blob associated visitors
mola (ocean sunfish), thresher sharks, etc. both are often associated with warmer waters.
ocean acidification
carbon dioxide can dissolbe in water.
- carbonated drinks: pressurized CO2 is dissolved in water. when opened at normal pressure, it releases CO2 bubbles.
- higher atmospheric CO2 means more CO2 dissolves in seawater.
chemistry of ocean acidification
when CO2 is dissolved in water, some carbonic acid is formed (H2CO3). water becomes more acidic (less basic). the pH of the ocean has been decreasing as CO2 levels have risen.
ph scale
7: pure water
8. 16: sea water (historical)
2050: 7.95
2100: 7.82