FLEXE Great Tubeworm Mysteries How can animals like the giant tubeworm exist in the cold dark seafloor?

Slides:



Advertisements
Similar presentations
Cold Seep Research at MBARI S. Goffredi and V. Orphan.
Advertisements

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.
CHEMOSYNTHESIS Who’d a thunk it?. Chemosynthetic bacteria  The basis for all life at hydrothermal vents.  Archaea – very primitive, different from other.
FROM THE MIDOCEAN RIDGES TO THE BLACK SMOKERS. What is it a midocean ridge? A midocean ridge it’s due to the divergence between two plates (e.g. The African.
Chemosynthesis and Hydrothermal Vents
Investigating chemosynthesis
Geol104/BioES154 Deep-Sea Hydrothermal Vent Communities.
Deep Sea 016b. 100m dysphotic aphotic photic Deep Ocean Characteristics Cold Still Stable Dark Essentially no productivity Sparse Life Extremely high.
Objective: Students will know that producers provide energy for other organisms in an ecosystem AND that almost all producers obtain energy from sunlight.
Deep-Sea Hydrothermal Vent Communities
Provides Energy to make LIFE possible!
An Overview of Photosynthesis. The Big Picture All organisms need energy to carry out essential functions (growth, movement, maintenance, repair, reproduction).
Photosynthesis and Cellular Respiration. Photosynthesis Definition: process in which plant cells convert the energy from sunlight into chemical energy.
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.
Animal Nutrition III (Ch. 41). Keywords Ruminant digestion Symbiosis –Definition –Algal-invertebrate –Chemoautotroph- invertebrate Hydrothermal vent H.
Converting Light Energy into Chemical Energy
Chemical Energy and ATP
Energy Transfer In Plants Changing the Sun’s Energy Into Useable, Stored Energy.
Photosynthesis Section Leaf structure Pigments and Sunlight Chlorophyll reflects green and some blue and yellow light while it absorbs the energy.
Hydrothermal Vent Bacteria that live near hydrothermal vents.
Energy Flow In Ecosystems
The Carbon and Oxygen Cycles
The process of photosynthesis: 6CO2 + 6H2O C6H12O6 + 6O2 Carbon Water sugar oxygen Dioxide (chemical energy)
Types of Nutrition and Photosynthesis
Energy Learning Objectives Define autotroph and heterotroph
Ch.26/27. I. History of life A. Earth formed about 4.5 billion years ago B. Life began a few 1,000,000 years later 1. Metabolic activity found in 3.5.
4.1 Chemical Energy & ATP 4.2 Overview of Photosynthesis 4.3 Photosynthesis in Detail CELL ENERGY.
Zones of the Ocean. It’s all just one big ocean!
Hydrothermal Vents and Deep Sea Exploration
HYDROTHERMAL SPRINGS & "VENT" COMMUNITIES OF MID-OCEAN RIDGES
Flabby Whalefish Blob Fish Hydrothermal Vent Tongue Fish.
Deep Ocean. 
Chapter 8: Photosynthesis
 What are the most important energy sources in foods you eat?  Carbohydrates and lipids.
Photosynthesis Takes place only in autotrophs (make their own food) (e.g. plants, Archaea, also some Protists and Bacteria) Basically, light energy is.
Hydrothermal Vents: Frontiers in Ocean Discovery.
The ability to create energy from the sun and Carbon Dioxide.
13.2 Biotic and Abiotic Factors Every ecosystem includes both living and nonliving factors.
Lesson Overview 3.2 Energy, Producers, and Consumers.
© 2014 Pearson Education, Inc. Chapter 15 Animals of the Benthic Environment Rocky and sandy shores Coral Reef Deep Sea.
Photosynthesis and Cellular Respiration Extra Notes.
Chapter 8: Energy and Photosynthesis
Without it there would be no life at the bottom of the sea
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.
Hydrothermal vents: Life in the hot, deep sea
Autotrophs vs Heterotrophs
Energy in Ecosystem Notes
Life Processes Life began in the ocean
Hydrothermal Vents
How do organisms get food?
Photosynthesis 1.
Energy Energy.
The Ocean.
KEY CONCEPT Life in an ecosystem requires a source of energy.
Benthic Zone (Deep Ocean)
KEY CONCEPT Life in an ecosystem requires a source of energy.
How deep can we go? Part 2.
KEY CONCEPT Life in an ecosystem requires a source of energy.
Photo by Thomas Dreps Energy Conversions Glucose ATP.
Autotrophs vs Heterotrophs
KEY CONCEPT Life in an ecosystem requires a source of energy.
Photo by Thomas Dreps Energy Conversions Glucose ATP.
KEY CONCEPT Life in an ecosystem requires a source of energy.
Photosynthesis Part 2.
Photo by Thomas Dreps Energy Conversions Glucose ATP.
KEY CONCEPT Life in an ecosystem requires a source of energy.
KEY CONCEPT Life in an ecosystem requires a source of energy.
KEY CONCEPT Life in an ecosystem requires a source of energy.
KEY CONCEPT Life in an ecosystem requires a source of energy.
Energy Transfer In Plants
Presentation transcript:

FLEXE Great Tubeworm Mysteries How can animals like the giant tubeworm exist in the cold dark seafloor?

FLEXE Great Tubeworm Mysteries Tubeworms were first discovered at Mid-Ocean Ridges (Image from U.S. Geological Survey) Locations of Mid-Ocean Ridges

(Image from Dive and Discover, WHOI) FLEXE Great Tubeworm Mysteries Mid-Ocean Ridge Processes Spreading Centers Ocean Bottom

FLEXE Great Tubeworm Mysteries Global distribution of known hydrothermal vent sites (Image from Van Dover et al. 2002)

How hydrothermal vents form FLEXE Great Tubeworm Mysteries (Image from Dive and Discover, WHOI) Deep Ocean Seawater Seafloor

Scientists expected to find very little life at vents No light Very high pressure Low temperatures Very little food New seafloor Potential challenges: FLEXE Great Tubeworm Mysteries

But THIS is what they found instead! FLEXE Great Tubeworm Mysteries What are these animals eating?

And so began the Great Tubeworm Mystery… Before you begin to solve the mystery, let’s look at what scientists did know about the vent environment. FLEXE Great Tubeworm Mysteries

Bacteria are everywhere!! (Image courtesy of Dr. Joe Resing and WHOI) FLEXE Great Tubeworm Mysteries

Some bacteria can perform chemosynthesis Photon Energy Reduced chemical (often sulfide, HS - ) Oxidized chemical Chemosynthesis: CO 2 + H 2 O  sugars + O 2 Photosynthesis: Chemical Energy FLEXE Great Tubeworm Mysteries

But back to the tubeworms Mystery: How do the tubeworms obtain nutrition? Hypothesis #1: Tubeworms are eating free-living bacteria to obtain energy. FLEXE Great Tubeworm Mysteries

No Mouth No Digestive Tract No Anus Basic Tubeworm Anatomy But how can they eat with no mouth, gut, or anus? FLEXE Great Tubeworm Mysteries

Basic Tubeworm Anatomy Dr. Colleen Cavanaugh used microscopy techniques in 1981 and discovered billions of bacterial cells packed inside the tubeworm’s trophosome bacteria per gram of trophosome!! Plume Trophosome Lines of evidence - #1 FLEXE Great Tubeworm Mysteries

Also in 1981, Dr. Horst Felbeck discovered Rubisco, the same enzyme plants use in the Calvin Cycle in photosynthesis, in the tubeworm. Lines of evidence - #2 FLEXE Great Tubeworm Mysteries Rubisco Calvin Cycle INPUT = inorganic carbon OUTPUT = organic carbon Sugar enzymes and chemical reactions CO 2

H 2 S from vent fluids 3. Sugars from bacteria are used as food by tubeworm Tubeworm + bacteria = Symbiosis! FLEXE Great Tubeworm Mysteries 2. Bacteria in trophosome use H 2 S, CO 2, and O 2 to make sugars via chemosynthesis 1. Tubeworm takes up hydrogen sulfide (H 2 S), carbon dioxide (CO 2 ) and oxygen (O 2 ) using its plume and shuttles these chemicals to its trophosome CO 2 and O 2 from seawater

The Mystery Continues … Mystery: What about tubeworms found at cold seeps? Hypothesis #2: Seep tubeworms obtain energy in the same way as vent tubeworms. FLEXE Great Tubeworm Mysteries

Cold seeps support lush communities Scientists assumed that seep tubeworms would obtain their energy the same way vent tubeworms do because: 1. Seep tubeworms have plumes 2. Seep tubeworms have trophosomes packed full of bacteria that use sulfide as an energy source FLEXE Great Tubeworm Mysteries

Energy sources in the Gulf of Mexico FLEXE Great Tubeworm Mysteries Salt layer Sediment layer Rock (shale) layer Ocean Sulfate in seawater sulfide methane methane Bacteria in the sediment use the energy obtained by oxidizing methane to create sulfide from sulfate Hydrocarbons (Methane) Seep tubeworm community

Plume level: No sulfide (0 µM H 2 S) Sulfide measurements around tubeworms Height of tubeworms = ~ 1 meter Mid-level: Very low sulfide ( µM H 2 S) Sediment level: Low sulfide (0 - 1 µM H 2 S) In the sediment: Very high sulfide levels ( ,000 µM H 2 S) FLEXE Great Tubeworm Mysteries Levels of Sulfide (H 2 S) at Cold Seeps

The Mystery Continues … Mystery: How do seep tubeworms take up sulfide? Hypothesis #3: What do you think??? FLEXE Great Tubeworm Mysteries

Mystery Solved! These tubeworms have ‘roots’! (well, not true roots, but extensions of their bodies that look and act like roots) 1. Sulfide from the sediment is taken up by the tubeworm extensions (‘roots’) 2. Sulfide is then transferred to the symbiotic bacteria in the trophosomes of the tubeworms FLEXE Great Tubeworm Mysteries In the sediment: Very high sulfide levels ( ,000 µM H 2 S)