1. On tectonic plate boundaries, magma seeps from the mantle into layers of rock closer to the crust.
Smokers:
- larger chimneys
- hotter temperatures
- release iron, sulfur
4
2. Ocean water seeps into cracks in the ocean floor.
BLACK vs. WHITE
Hydrothermal Vent Ecology
5
- smaller chimneys
- cooler temperatures
- release barium, calcium, silicon
3. Percolating water is superheated by underlying magma; at the same time, it dissolves minerals in the surrounding rock layer.
2
3
4. Water and dissolved minerals are expelled from the vent in a plume of scorching liquid.
Where can you find them?
1
Along plate boundaries in the oceanic crust . . .
5. Minerals and compounds settle on the ocean floor, creating structures called "chimneys" and providing an energy source for local life.
Molly Cunningham
Hydrothermal Vent Geology
all consumers
Chemosynthesis
In the absence of sunlight, deep sea producers must use alternative processes to build organic matter.
VULCANOCTOPI
More energy produced from oxidative phosphorylation
COPEPODS
BUT
AEROBIC
Higher energy cost to synthesize carbohydrates
AEROBIC
ANAEROBIC
ENERGY TRADEOFFS
PHOTO
Comparing
EXCEPT . . .
The bacterium GSB1, which photosynthesizes off of the light given off by its black smoker . . .
ANAEROBIC
- Found in virtually all plant life
The only organism known to photosynthesize with anything other than solar light!
Less energy produced from electron transport chain with less electronegative acceptor
- Occurs in chloroplasts (eukaryotes) and cytoplasm (prokaryotes)
. . .not photosynthesis!
BUT
In environments where oxygen is present. . .
Lower energy cost to synthesize carbohydrates
- Utilizes but does not depend on symbiosis
- convert energy into usable compounds
- use an electron transport chain
- found in bacteria and archaea
CHEMO
- Found in only bacteria and archaea
CO + H O + H S + O CH O + H SO
2
4
Electron Transport Chain
- Harnesses geothermal energy
- Occurs in only prokaryotes
- consume crabs, tubeworms
- can reach over one meter in length
- demonstrate convergent evolution with eels
Electron donor:
Electron acceptor:
- Requires symbiosis to create a functional ecosystem
H S + 6H O + CO C H O + 6O
2
6
12
6
2
O
Sulfide ions
- parasites to vulcanoctopi and zoarcid fish
- latch on to flesh of hostith claws on antennae
2
in the oxygen-free environment characteristic of black smokers . . .
Electron Transport Chain
- named so because of activity with hydrothermal vents (which are technically a type of volcano)
- sightless--use arms to detect, wrangle, and eat crustaceans
- translucent--never evolved crypsis (color-changing camouflage trait)
- engage in commensalism with tubeworms, using them for shelter
Carbon Fixation
Calvin Cycle
-7 ATP
Electron acceptor:
Electron donor:
CO to make sugars
2
fumarate
3+
Fe
Well . . .
sulfide ions
ZOARCID FISH (EELPOUTS)
NO
3
4+
Reductive TCA Cycle = a reverse Krebs cycle
Mn
CO + H O = organic compounds
2
-2 ATP
SO
Wood-Ljungdahl Pathway = reductive carboxylation
Carbon Fixation
2
- CO to make Acetyl CoA
- adds carboxyl end to compounds to produce pyruvate
-1 ATP
SHRIMP
- blind
- detect dead material with feelers on the ocean floor
- actually several small, tube-like organisms that travel in clusters
- evolutionarily related to jellyfish
- use long tentacles to detect food, anchor unit on rocks, move
- usually the last to arrive to a vent site--lots of dead material, usually signifies "dying" vent
DECOMPOSERS
SQUAT LOBSTERS
CONSUMERS
SEA DANDELIONS
THERMOTOGALES BACTERIA
- actually crabs
- secondary consumers--scavengers
- engage in commensalism with tubeworms, using them for shelter
- single-unit lipid membrane
- consume carbohydrates and produce hydrogen gas
- possible biofuel source
LIMPETS
MUSSELS
TUBEWORMS
- snail-like organisms
- consume algae
CLAMS
Why are
HYDROTHERMAL VENT COMMUNITIES
SOURCES
- http://www.whoi.edu/oceanus/feature/deep-sea-tubeworms-get-versatile-inside-help
- http://divediscover.whoi.edu/vents/biology.html
- http://scienceblogs.com/deepseanews/2007/04/11/from-the-desk-of-zelnio-vulcan/ file:///C:/Users/molly_000/Downloads/HuglerSeifert10_AnnRevMar.pdf
- https://www.cambridge.org/core/journals/parasitology/article/deepsea-hydrothermal-vent-parasites-why-do-we-not-find-more/CBBFCF40571670549A6F4DA7762F7708
- http://www.vims.edu/~jeff/biology/2005%20Hoeg%20et%20al.%20Ecol.%20Mar.%20Parasites%20-%20parasitic%20crustaceans.pdf
- https://www.ncbi.nlm.nih.gov/pubmed/18664307
- http://aem.asm.org/content/71/4/1694.fullfile:///C:/Users/molly_000/Downloads/HuglerSeifert10_AnnRevMar.pdf
They give insight on life in the absence of oxygen and sunlight!
- very similar to mussels--main difference is rounded, white shell
- bacteriophytes
- gills and filter-feeding
- share special enzyme with mussels and tubeworms that allow for thriotrophic endosymbiosis--evolutionary connection
significant to biology?
They provide a completely closed and isolated system for ecological study!
some endosymbionts in tubeworms have even demonstrated the ability to switch carbon fixation cycles depending on oxygen availability!
- have no digestive tract, must live completely off of endosymbiosis with bacteria
- bacteria enter the "tube" via trophosomes on the surface of the skin
- red plumes = gills, hemoglobin (responsible for red color) transports absorbed nutrients to endosymbionts
They present opportunities in biofuel research!
They demonstrate the ability of life to thrive even at extreme temperature and under extreme pressure!
- live off of filter-feeding and endosymbiosis
- house endosymbionts in gills in membrane-enclosed vacuoles called "bacteriophytes"
- appear at a hydothermal vent site after tubeworm colonies have developed
THEY'RE F***ING SICK!!!!!!!!!!!
PRODUCERS
ARCHAEA
all producers
- methanotrophic or thriotrophic prokaryotes
- organisms like these are hypothesized to be the origin of life
BACTERIA
- also methanotrophic or thriotrophic prokaryotes