Climate and Biomes IV. Aquatic Systems. Climate and Biomes IV. Aquatic Systems A. Overview Characterized by physical characteristics and general biological.

Slides:



Advertisements
Similar presentations
The Marine Biome.
Advertisements

The Aquatic Environment. Estuaries A coastal body of water surrounded by land with access to the open ocean. A coastal body of water surrounded by land.
Chapter 6 Aquatic Biodiversity
Lesson Overview 4.5 Aquatic Ecosystems.
Aquatic Ecosystems.
Ecology 15 Freshwater, Marine and Wetland Systems Global Climate Change Ralph Kirby.
ECOLOGY AND THE BIOSPHERE
Compare and Contrast What are some ways in which life in an aphotic zone might differ from life in a photic zone Apply Concepts What is a wetland and.
50.3 Abiotic and biotic factors influence the structure and dynamics of aquatic biomes. 30  N Tropic of Cancer Equator 30  S Contine ntal shelf Lakes.
Lesson Overview 4.5 Aquatic Ecosystems.
Aquatic Ecosystems Chapter 54. In general…  Aquatic ecosystems are classified primarily on abiotic factors: temperature, salinity, dissolved oxygen,
Aquatic Biomes This can be found on my website. What factors influence the kind of life an aquatic biome contains?   Salinity (how much salt)   Depth.
Aquatic Ecosystems Determining factors:
Aquatic Ecosystems make up most of the Biosphere
Chapter 5 Aquatic Ecosystems.
Biomes Biotic & Abiotic Factors Terrestrial Biomes Aquatic Biomes Biotic & Abiotic Factors Terrestrial Biomes Aquatic Biomes.
End Show Slide 1 of 39 Copyright Pearson Prentice Hall biology.
Warm-up Compare the answers you have on your Planet Earth worksheets with others at your table.
Freshwater Ecosystems and Succession. Freshwater Ecosystems Two broad categories: – Stationary Water  Lakes, Ponds, and Reservoirs – Running Water (Downhill)
Aquatic Ecosystems Chapter 7.
Aquatic Biomes. Salt in Water Most of the salt in oceans is carried in by rivers.
Aquatic Biomes Categorized by depth, salinity, temperature, dissolved oxygen Freshwater : streams, rivers, lakes and wetlands Marine: estuaries, intertidal.
Copyright Pearson Prentice Hall
Aquatic biomes are categorized by: Salinity Freshwater Saltwater (marine) Depth Water flow.
 The study of fresh bodies of water  Lentic: standing water (lakes and ponds)  Lotic: flowing water (streams and rivers)
1 Life in Water Chapter 3. 2 The Hydrologic Cycle Over 71% of the earth’s surface is covered by water:  Oceans contain 97%.  Polar ice caps and glaciers.
Aquatic Ecosystems. ¾ of earth is covered by water Two types of aquatic ecosystems: Freshwater ecosystems Marine ecosystems.
CHAPTER 50 AN INTRODUCTION TO ECOLOGY AND THE BIOSPERE Copyright © 2002 Pearson Education, Inc., publishing as Benjamin Cummings Section C1: Aquatic and.
Lesson Overview Lesson Overview Aquatic Ecosystems Lesson Overview 4.5 Aquatic Ecosystems.
Aquatic Ecosystems. Occupy largest part of biosphere Two major categories: Freshwater Marine.
Aquatic Biomes.
Aquatic Life Zones Aquatic biomes are categorized by: Salinity Depth
© 2012 John Wiley & Sons, Inc. All rights reserved. Freshwater Ecosystems  Includes:  Rivers and streams  Lakes and ponds  Marshes and swamps  Represent.
CHAPTER 52 An Introduction to Ecology and the Biosphere.
Water Biomes Biology Unit 14 Notes Water Biomes   Water biomes are differentiated by several abiotic factors: Light Temperature Amount of salt.
Aquatic Biomes Earth's Aquatic Biomes Aquatic biomes cover approximately three-fourths of the Earth's surface and are connected to terrestrial and other.
Biomes and Aquatic Ecosystems
Lecture 14 Freshwater Ecosystems Ozgur Unal
Copyright Pearson Prentice Hall
Aquatic Ecosystems.
Chapter 6-AQUATIC Biomes Major Ecosystems of the World
Categorized by depth, salinity, temperature, dissolved oxygen
Water and Aquatic Biomes
Freshwater Ecosystems Notes
Section 3: Aquatic Ecosystems
Section 3: Aquatic Ecosystems
Aquatic Ecosystems Chapter 7.
Lesson Overview 4.5 Aquatic Ecosystems.
Aquatic Biomes.
Biomes & Aquatic Ecosystems.
Freshwater Ecosystems
4-5 Aquatic Ecosystems Photo Credit: © Belinda Wright/DRK Photo.
By: Lauren Clark Aquatic Biomes.
Chapter 7 Major Ecosystems of the World
Diagram.
Biomes A BIOME is a large group of ecosystems that share the same kind of climax community. There are 2 Types of Biomes: Terrestrial Aquatic.
Copyright Pearson Prentice Hall
4-4 Aquatic Ecosystems Water covers ¾ of Earth, has an average depth of 3.7 (deepest part is 11 km – 6.8 mi) miles, contains about 3% salt and only 3%
Module 13 Aquatic Biomes After reading this module you should be able to Identify the major freshwater biomes. Identify the major marine biomes.
List the major land biomes.
Section 3: Aquatic Ecosystems
Copyright Pearson Prentice Hall
Objective: Students will explore characteristics of aquatic ecosystems in order to explain the importance of coral reefs and wetlands. Drill: 11/09/16.
Aquatic Biomes are Categorized by Salinity, Depth, and Water Flow
Lesson Overview 4.5 Aquatic Ecosystems.
Chapter 4.4 Aquatic ecosystems.
4:4 Aquatic Ecosystems Water covers ¾ of Earth, has an average depth of 3.7 (deepest part is 11 km – 6.8 mi) miles, contains about 3% salt and only.
Ecosystems.
Aquatic Ecosystems.
Copyright Pearson Prentice Hall
Presentation transcript:

Climate and Biomes IV. Aquatic Systems

Climate and Biomes IV. Aquatic Systems A. Overview Characterized by physical characteristics and general biological parameters like productivity, not plant growth form (algae)

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams Where precip > evaporation, excess soil water runs to water table. Where water table is expressed above land = stream.

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams - High gradient

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams - High gradient - low primary productivity; no upstream source of nutrients, organics from riparian zone (allochthonous)

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams - High gradient - low primary productivity; no upstream source of nutrients, organics from riparian zone (allochthonous) - usually with a complete canopy that reduces photosynthesis

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams - High gradient - low primary productivity; no upstream source of nutrients, organics from riparian zone (allochthonous) - usually with a complete canopy that reduces photosynthesis - sequence of riffle (production) and pool (decomposition)

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams - High gradient - low primary productivity; no upstream source of nutrients, organics from riparian zone (allochthonous) - usually with a complete canopy that reduces photosynthesis - sequence of riffle (production) and pool (decomposition)

- Communities driven by detritivores consuming allochthonous inputs, not aquatic primary productivity

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers Rivers = order 6-12 Ohio = 8 Mississippi = 10 Amazon = 12

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers - lower gradient; more volume and force

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers - lower gradient - Higher productivity, fed by nutrients from upstream - wider waterway allows sunlight to feed local productivity and decomposition (autochthonous)

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers - lower gradient - Higher productivity, fed by nutrients from upstream - wider waterway allows sunlight to feed local productivity and decomposition (autochthonous) - meanders dominate, creating lateral habitats from cut bank and pool to sand bar and riffle across the course of the river.

Oxbow Lake

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers - lower gradient - Higher productivity, fed by nutrients from upstream - wider waterway allows sunlight to feed local productivity and decomposition (autochthonous) - meanders dominate, creating lateral habitats from cut bank and pool to sand bar and riffle across the course of the river. - in large, deep rivers, the amount of sediment carried in the river, coupled with water depth, may reduce algal photosynthesis at depth and decrease productivity.

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers

a.Headwater Streams b.Rivers River Continuum Concept Moving downstream: -NPP increases, changes from periphyton (attached algae) to phytoplankton (floating). -Proportional E input by CPOM declines, shredders decline. -FPOM and UFPOM increase, and collectors (filterers) increase -“downstream succession” of increasing productivity -Upstream, P/R < 1 -Downstream, P/R > 1

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers c.Marshes and Swamps - these are habitats that are flooded periodically, either by rainfall, rivers, or tidal inundation (though these would be saline salt marshes).

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) a.Headwater Streams b.Rivers c.Marshes and Swamps - They are highly productive habitats, receiving nutrients from both aquatic and terrestrial sources. They are often shallow, also, so there are high autochthonous productivity. This high biological productivity can reduce oxygen levels in the water and sediment, however. Also, the high biological activity serves to detoxify and filter surface and ground water.

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) 2. Lentic Systems a. Lakes - temporary habitats, as they will eventually fill with sediment carried by stream inputs or surface runoff. - formed by natural dams (beaver, mudslide), glacial retreat, limestone erosion, changes in river channels (oxbows), continental drift (rift lakes), and man-made dams

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) 2. Lentic Systems a. Lakes - Littoral Zone: edge with rooted plants - Limnetic/Pelagic Zone: no rooted plants; in deep lakes this may be further subdivided -subdivided by temperature stratification: epilimnion thermocline hypolimnion -subdivided by light penetration: euphotic zone compensation depth aphotic zone - Benthic zone: sediments where decomposition occurs and nutrients accumulate

Lentic Systems: Ponds and Lakes

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems (moving waters) 2. Lentic Systems a. Lakes - In deep lakes, the spatial separation of nutrients beneath the photic zone means that algae are nutrient limited until turnover occurs in fall and spring. - Deep lakes often have low productivity = oligotrophic. Shallow lakes have more productivity = eutrophic. The release of nutrient limitation – eutrophication.

IV. Aquatic Systems B. Freshwater Habitats 1. Lotic Systems 2. Lentic Systems b. Ponds and bogs -A smaller water body, often later in lake succession: Lake Pond Bog Marsh Meadow

IV. Aquatic Systems C. Marine Habitats 1. Estuaries - Place where rivers meet the ocean; often made discrete by barrier islands offshore.

IV. Aquatic Systems C. Marine Habitats 1. Estuaries - Place where rivers meet the ocean; often made discrete by barrier islands offshore. - direction of water flow, depth, and salinity changes with the tides

IV. Aquatic Systems C. Marine Habitats 1. Estuaries - highest productivity aquatic habitat; nutrients accumulate and feed surrounding salt marshes or mangroves, which add nutrients to the estuary. Truly a highly connected mix of terrestrial, marine, and aquatic habitats.

IV. Aquatic Systems C. Marine Habitats 1. Estuaries 2. Intertidal (littoral) - habitat between high and low tide - zonation of organisms based on desiccation tolerance and frequency and length of exposure.

IV. Aquatic Systems C. Marine Habitats 1. Estuaries 2. Intertidal (littoral) 3. Neritic Zone (Cont. Shelf) - usually to a depth of 200m - productive because benthic nutrients are close to the photic zone and the habitat is well mixed.

Marine Systems

IV. Aquatic Systems C. Marine Habitats 1. Estuaries 2. Intertidal (littoral) 3. Neritic Zone (Cont. Shelf) 4. Oceanic (Pelagic) - open ocean to depth of 5 miles in trenches. - photic and aphotic zones - very low productivity except in upwelling areas where nutrients are brought up into the photic zone, or hydrothermal vent communities where chemosynthetic bacteria are the primary producers.

IV. Aquatic Systems C. Marine Habitats 1. Estuaries 2. Intertidal (littoral) 3. Neritic Zone (Cont. Shelf) 4. Oceanic (Pelagic) 5. Coral Reefs - typically shallow, tropical habitats with high productivity of algal symbiots in coral polyps. - also, structural complexity of the reef increases habitat variation and diversity. - most diverse marine systems.

IV. Aquatic Systems C. Marine Habitats 1. Estuaries 2. Intertidal (littoral) 3. Neritic Zone (Cont. Shelf) 4. Oceanic (Pelagic) 5. Coral Reefs 6. Hydrothermal Vent Communities - primary producers are chemosynthetic sulphur bacteria; some of which have become endosymbionts of giant polychaete worms (Riftia sp.).