How deep can we go? Part 2.

Slides:



Advertisements
Similar presentations
Do Now Think about what you had for breakfast this morning. Think about what you had for breakfast this morning. Where did it come from? Where did it come.
Advertisements

CHEMOSYNTHESIS Who’d a thunk it?. Chemosynthetic bacteria  The basis for all life at hydrothermal vents.  Archaea – very primitive, different from other.
Ocean Water and Ocean Life
15. 2 Diversity of Ocean Life & 15.3 Oceanic Productivity
Investigating chemosynthesis
Bellwork 12/15 Answer in notebook: 1. What is necessary for humans to live? 2. Where do humans get the things they need to survive? 3. What sort of impact.
POWER FOR LIFE’S PROCESSES Energy Flow. Producers Sunlight is the primary source of energy source for life on earth. Plants, algae, and some bacteria.
Objective: Students will know that producers provide energy for other organisms in an ecosystem AND that almost all producers obtain energy from sunlight.
The Diversity of Ocean Life
Ocean Zones & Layers The ocean is divided into three zones across and three layers down. Use the diagram on the next slide to label the diagram on your.
Marine Zones iNOB.
Conditions differ away from shore.
CHAPTER 15 Animals of the Benthic Environment
Abyssal Zone Zone on the Bottom of the Ocean. The ocean zone where you would find organisms such as worms, sea urchins, and chemosynthetic bacteria.
OCEAN ECOSYSTEMS Powered by solar energy, with sunlight driving photosynthesis by phytoplankton.
Energetics of Marine Ecosystems Part I
Life Away From Shore Ocean life differs farther away from shore.
Chapter 5 - Section 1 Energy Flow In Ecosystems. Ecosystem = interacting system that involves both organisms and their nonliving environment includes….
Zones are classified by depth and by how much light penetrates
Converting Energy Matter and energy move through the natural world in different ways. Matter can be recycled over and over again. Energy Flow 3 3 The.
FOOD CHAINS & FOOD WEBS. FOOD CHAINS vs. FOOD WEBS FOOD CHAIN – Diagram that shows how energy flows from 1 organism to another in an ecosystem. FOOD WEB.
Energy Flow In Ecosystems
D IVERSITY & PRODUCTIVITY OF O CEAN L IFE.  Classification is a way of organizing living things  Things that live in the ocean are called marine organism.
15 Chapter 15 Ocean Water and Ocean Life The Composition of Seawater  Salinity is the total amount of solid material dissolved in water.  typically.
What Ocean zone is closest to the shore?  Intertidal Zone  Why do we call the shoreline an INTERTIDAL zone?  **Because it is where land and sea meet.
The Carbon and Oxygen Cycles
Energy Learning Objectives Define autotroph and heterotroph
Zones of the Ocean. It’s all just one big ocean!
Open Ocean Notes 1. How is the open ocean different from the neritic zone?  Less sunlight—Surface Zone (200 m) is only layer the sun penetrates  The.
Environments and Primary Productivity. Environments Pelagic……the water Neritic – over continental shelf Oceanic Epipelagic: down to 200 m Mesopelagic:
Deep Ocean. 
Main Idea #1: Ocean life changes as you move from the shoreline out to open ocean Main Idea #2: Ocean life changes as you move from the surface to the.
Conditions away from shore ● Closest to the shore is the Continental shelf ● Sunlight reaches almost to the bottom of the Continental shelf ● Nutrients.
Ecology: Chapter 3. What is Ecology? Ecology – study of interactions among organisms and between organisms & their environment All living things depend.
Ocean Zones & Layers The ocean is divided into three zones across and three layers down. Use the diagram on the next slide to label the diagram on your.
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Bell Ringer What does an organism need to survive? Where does life on earth begin? Can you think of life that does not begin with the sun?
Hydrothermal Vents By Taylor, Jarrad and David What are Hydrothermal Vents A hypothermal vent is based on the ocean floor and is known as a hot spring,
Salinity Salinity is the total amount of solid material dissolved in water. Because the proportion of dissolved substances in seawater is such a small.
Chapter 15. Salinity Chemical weathering on land creates chemicals picked up by freshwater and delivered to the ocean Mainly sodium chloride Chemicals.
© 2014 Pearson Education, Inc. Chapter 15 Animals of the Benthic Environment Rocky and sandy shores Coral Reef Deep Sea.
Marine Life.
18.2 The Carbon and nitrogen cycle
THE OCEAN DEPTHS.
What Shapes an Ecosystem?
OCEAN WATER AND OCEAN LIFE
Warm-up Directions Take Cornell notes in your lab journal on slides #2 – 9. Turn the title into a question and summarize the information on each.
The Diversity of Ocean Life
Energetics of Marine Ecosystems Part I
The Sea Floor or Ocean Basins
KEY CONCEPT Marine ecosystems are global. 70% of Earth’s surface is
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Deep Ocean Zone and Ocean Exploration
Review of the ocean zones
Hydrothermal Vents
Review of the ocean zones
Energy Energy.
Ocean Exploration & Technologies NOTES
3.2 Energy, Producers, and Consumers
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Vent Tubeworm Vent Amphipod
Our ocean has 3 zones:. What kind of living things we find depends upon where we are in the ocean.
Energetics of Marine Ecosystems Part I
Photo by Thomas Dreps Energy Conversions Glucose ATP.
Interesting Food Webs.
Photo by Thomas Dreps Energy Conversions Glucose ATP.
Photo by Thomas Dreps Energy Conversions Glucose ATP.
Ocean Ecosystems Vocabulary…98
6e. Know a vital part of an ecosystem is the stability of its producers and decomposers. 3–2 Energy Flow.
The Discovery of Ocean Life
Presentation transcript:

How deep can we go? Part 2

Let’s review…

The deep ocean zone (BENTHIC zone) is the LARGEST sized ocean ____________ by far! Because of crushing pressure, darkness, and its huge size, most of it is unexplored!

The deep ocean zone (BENTHIC zone) is the LARGEST sized ocean ECOSYSTEM by far! Because of crushing pressure, darkness, and its huge size, most of it is unexplored!

A greatest ________ of life exists in the ABYSS! http://news.discovery.com/animals/deep-sea-amoeba-life- 111023.html

A greatest VARIETY of life exists in the ABYSS! http://news.discovery.com/animals/deep-sea-amoeba-life- 111023.html

A greatest VARIETY of life exists in the ABYSS! http://news.discovery.com/animals/deep-sea-amoeba-life- 111023.html

The greatest variety of life exists in the ABYSS! http://news.discovery.com/animals/deep-sea-amoeba-life- 111023.html

Still, the ___________ coast & especially the ___________ continental shelf have lots of ocean life! Especially during _____________! LOTS of GOOEY EDIBLE MUCK…mmmmmm

Still, the INTERTIDAL coast & especially the NERITIC continental shelf have lots of ocean life! Especially during UPWELLING! LOTS of GOOEY EDIBLE MUCK…mmmmmm

The intertidal and neritic zones have lots of life because of the _ _ _ ! The _ _ _ kicks off ______________!

The intertidal and neritic zones have lots of life because of the SUN! The sun kicks off PHOTOSYNTHESIS!

The INTERTIDAL and NERITIC zones still have plenty of life of their own because of the SUN! The sun kicks off PHOTOSYNTHESIS!

With PHOTOSYNTHESIS, most producers (kelp, phytoplankton like _____) can make their OWN _____ food!

With PHOTOSYNTHESIS, most producers (kelp, phytoplankton like algae) can make their OWN sugar food!

Sometimes _____ can run AMOK Sometimes _____ can run AMOK! Usually because of run-off fertilizers from land _____.

Sometimes algae can run AMOK Sometimes algae can run AMOK! Usually because of run-off fertilizers from land farms. eeeeeEUTROPHICATION

Sometimes algae can run AMOK Sometimes algae can run AMOK! Usually because of run-off fertilizers from land farms. eeeeeEUTROPHICATION

But there is no _____ in the deep zone (aka benthic zone).

But there is NO SUN in the deep zone (aka BENTHIC).

WHAT IS THE energy source OF BENTHIC FOOD WEBS? Without the SUN, WHAT IS THE energy source OF BENTHIC FOOD WEBS?

Got any ideas? It can’t get it’s energy from the sun!

How does life start in the ABYSS? CHEMICAL ENERGY ! (not solar energy) http://hubpages.com/education/What-are- Chemosynthetic-Bacteria

How does life start in the ABYSS? CHEMICAL ENERGY ! (not solar energy) HYDROTHERMAL VENTS spew H2S for CHEMOSYNTHESIS!

How does life start in the ABYSS? CHEMICAL ENERGY ! (not solar energy) HYDROTHERMAL VENTS spew H2S for CHEMOSYNTHESIS!

PHOTOSYNTHESIS…

http://hubpages.com/education/What-are-Chemosynthetic-Bacteria DROTHERMAL VENTS spew all sorts of gases for things to live on! Chemosynthetic bacteria use inorganic molecules as a source of energy including ____________ (NH3) , ___________(S) and __________ ____________ ( H2S ). Like their sun-loving photosynthesizers, chemosynthesizers are _____________ because they produce their own food. ____________ ________are located very deep into the ocean where sunlight is unable to penetrate; therefore, the organisms that live at ____________ ______ obtain their energy from the __________ ejected out from the ocean crust. Since the energy from the ____ cannot be used at such depths, the _______ ________ absorbs ___________ _________ (H2S) from the vent and provides it to the bacteria. So, these two living things have a ___________ MUTUALISTIC relationship.

http://hubpages.com/education/What-are-Chemosynthetic-Bacteria DROTHERMAL VENTS spew all sorts of gases for things to live on! Chemosynthetic bacteria use inorganic molecules as a source of energy including AMMONIA (NH3) , SULFUR (S) and HYDROGEN SULFIDE ( H2S ). Like their sun-loving photosynthesizers, chemosynthesizers are PRODUCERS because they produce their own food. HYDROTHERMAL VENTS are located very deep into the ocean where sunlight is unable to penetrate; therefore, the organisms that live at HYDROTHERMAL VENTS obtain their energy from the CHEMICALS ejected out from the ocean crust. Since the energy from the SUN cannot be used at such depths, the TUBE WORMS absorb HYDROGEN SULFIDE (H2S) from the vent and provides it to the bacteria. So, these two living things have a SYMBIOTIC MUTUALISITIC relationship because they help each other

Compare….

Do a VENN DIAGRAM PHOTOSYNTHESIS CHEMOSYNTHESIS Uses SUN for ENERGY! Uses CHEMICALS for ENERGY Absorbs CO2

Compare….

Do a VENN DIAGRAM PHOTOSYNTHESIS CHEMOSYNTHESIS Uses SUN for ENERGY! Produces oxygen (O2) for us to breathe Uses CHEMICALS for ENERGY Produces sulfuric acid, not oxygen Absorbs CO2 Living things produce own food (sugars/ carbs) to live on

Do a VENN DIAGRAM PHOTOSYNTHESIS CHEMOSYNTHESIS Uses SUN for ENERGY! Produces oxygen (O2) for us to breathe Phytoplankton & plants & trees Uses CHEMICALS for ENERGY Produces sulfuric acid, not oxygen Some bacteria & tube worms Absorbs CO2 Living things produce own food (sugars/ carbs) to live on Producers at the base of a food web

Do a VENN DIAGRAM PHOTOSYNTHESIS CHEMOSYNTHESIS Uses CHEMICALS for ENERGY Produces sulfuric acid, not oxygen Some bacteria & tube worms Found around HYDROTHERMAL VENTS at bottom Uses SUN for ENERGY! Produces oxygen (O2) for us to breathe Phytoplankton & plants & trees Absorbs CO2 Living things produce own food (sugars/ carbs) to live on Producers at the base of a food web

end

Life exists even in the ABYSS! HOW? CHEMICAL ENERGY ! (not solar energy) hydrothermal vents, submarine hot springs, and methane seeps; chemosynthetic organisms; dead stuff.

PRESS RELEASE Date Released: Tuesday, July 29, 1997 Source: Pennsylvania State University Methane Ice Worms Hesiocaeca methanicola (larger view) A team of university scientists using a mini research submarine on a NOAA-funded research cruise has discovered, photographed, and sampled what appears to be a new species of centipede-like worms living on and within mounds of methane ice on the floor of the Gulf of Mexico, about 150 miles south of New Orleans. Although scientists had hypothesized that bacteria might colonize methane ice mounds, called gas hydrates, this is the first time animals have been found living in the mounds. The discovery of dense colonies of these one-to-two-inch-long, flat, pinkish worms burrowing into a mushroom-shaped mound of methane seeping up from the sea floor raises speculation that the worms may be a new species with a pervasive and as yet unknown influence on these energy-rich gas deposits.

chemosynthesis vs. photosynthesis http://oceanexplorer.noaa.gov/edu/learning/player/lesson05/l5ex1.htm