DOC PREVIEW
CORNELL BIOEE 1610 - Deep Ocean Biome

This preview shows page 1 out of 3 pages.

Save
View full document
View full document
Premium Document
Do you want full access? Go Premium and unlock all 3 pages.
Access to all documents
Download any document
Ad free experience
Premium Document
Do you want full access? Go Premium and unlock all 3 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

Bioee 1610 1st Edition Lecture 5Outline of previous lectureI. FIRST PRELIM!II. Terrestrial biomesA) TundraB) Boreal forestC) Temperate forestD) Temperate grasslandE) MediterraneanF) DesertsG) Savanna/tropical seasonal forestH) Tropical rainforestOutline of current lectureI. ReminderII. Deep ocean biomeA) Deep oceanIII. Surface water biomesA) Subtropical gyresB) Upwelling systemsC) Continental shelvesD) High/low latitude watersE) SummaryCurrent lectureI. Reminder:*First test a week from today, during class (Feb 19)*Review session Wednesday Feb 18 6:30-8:30 in A106 Corson Hall (Bring questions!)*A-K in Plant Sciences 233*L-Z in Riley Robb*Professor will be gone for a couple weeks after test… we will have Professor Powers insteadII. Deep ocean biome*71% of earth, 97% of all water on earth*Freshwater biome information can be found in Essentials of Ecology*200m is the absolute lowest that light can reach into the water; in coastal waters it’s more like 50m or lessA) Deep ocean*Average depth of water=4.3km; max=11kmThese notes represent a detailed interpretation of the professor’s lecture. GradeBuddy is best used as a supplement to your own notes, not as a substitute.*Deep ocean=rivals the diversity of tropical rainforests (most organisms are tiny and slow)*No photosynthesis… where does the energy come from?-Chemoautotrophy-Sinking from surface waters*The deep ocean is around the 4-5 degrees Celsius (refrigerator temperature)*Low temperature=low bacteria activity, so animals eat a lot of the sinking organic matter *Carbon dioxide stored inorganically in the oceansIII. Surface water biomes*Defined by nutrient input, mostlyA) Subtropical gyres*Enclosed by currents*Cover half of the oceans’ surface area*Very high diversity*Productivity rivals the most arid of deserts*The water is really clear, so the light goes down 200m… why is there so little photosynthesis?-Very little nutrients (deeps ocean nutrients can’t reach them from below)*Low nutrients=small phytoplankton=long food chains (less efficient, so less production at top predators)*Sargasso sea  has Sargassum weed floating in sheets (creative name, right?)B) Upwelling systems*Upwelling – result of interaction of prevailing winds interact with coastlines; brings cold, deep-ocean water to surface*Light penetration is very low because there is so much phytoplankton*High productivity, low diversity*High nutrientslarge phytoplanktonshort food chainC) Continental shelves*High photosynthesis because they get a lot of nutrients from land*Low light penetration (often shallow so it doesn’t matter)*High productivity, relatively low diversityD) High/low latitude waters (Arctic, Antarctic)*Why would these waters be more productive than the gyres?-Less stratification= nutrients more readily available, but still light can reach far enough downE) Summary*Nutrient from land/river, but mostly deep ocean*Only in the top layer of the ocean is there enough light for photosynthesis*Compared to land: Photosynthesis is roughly equal on land and in the ocean, but biomass is greatest on land (remember, ocean surface is much greater thanland, but forests contain a whole lot of


View Full Document

CORNELL BIOEE 1610 - Deep Ocean Biome

Download Deep Ocean Biome
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Deep Ocean Biome and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Deep Ocean Biome 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?