The Open Ocean AKA EPIPELAGIC.

Slides:



Advertisements
Similar presentations
Epipelagic/Photic zone Surface to 200 m Surface to 200 m Warmest and best light for photosynthesis Warmest and best light for photosynthesis Divided into.
Advertisements

Biological Productivity. Conditions for Life in the Sea Consider the main biochemical reaction for life in the sea, and on earth in general: 6H 2 O +
Plankton Marine life is classified into three groups: Plankton, Nekton, and Benthos Plankton Nekton Benthos.
15. 2 Diversity of Ocean Life & 15.3 Oceanic Productivity
Epipelagic environment Upper pelagic –Surface to 200 m –Neritic Over continental shelf –Oceanic Beyond the shelf Correlates to the photic zone –Most of.
Chapter 15 Life Near the Surface.
The Nekton 1 What are Nektonic Animals? Organisms that have developed powers of locomotion Feeding Biology Practically all members of the nekton are carnivorous.
The Epipelagic The pelagic realm of the ocean describes the vast, open ocean. –The epipelagic realm is the upper part of this environment. Depths only.
OCEANIC LIFE ZONES.
Phytoplankton Dynamics Primary Productivity (g C/m 2 /yr) Gross (total) production = total C fixed Net production = C remaining after respiration Standing.
Honors Marine Biology Module 14
The uppermost layer of the world's oceans is bathed in sunlight during the daytime. photic zone, euphotic zone (euphotic means "well lit" in Greek) or.
Lecture 13 Export Production Lecture 12 summary: Primary Productivity is limited mostly by nutrients. In low latitudes (< 45 o ), the limiting nutrient.
Life Near the Surface Shipley Marine Biology Summit High School
OCEAN WATER.
QoD – Notes Allowed In your science notebook: 1) Freshwater coming in from rivers and precipitation causes slightly ________ salinity in seawater (choose.
Photic Pelagic Waters I. Location A. From surface to 200m (average) B. Where photosynthesis takes place.
Biological Productivity. Basic Ecology  physical and chemical parameters affecting distribution and abundance  An ecosystem includes both the living.
Chapter 15 Life Near the Surface. Pelagic – water column away from bottom or shore Pelagic – water column away from bottom or shore Epipelagic – sea surface.
Ocean Zones The Ocean is divided in three ways: The Water - Pelagic The Substrate (Ocean Floor) - Benthic Light Penetration – Photic/Aphotic.
Chapter 15.3 Oceanic Productivity. Marine organisms are connected through food production and consumption. Producers in the ocean are phytoplankton, larger.
Marine Ecology Chapter 10.
OCEANIC LIFE ZONES.
Marine Environments The environment itself Major groups of organisms in ocean Basics of ecosystems.
Environments and Primary Productivity. Environments Pelagic……the water Neritic – over continental shelf Oceanic Epipelagic: down to 200 m Mesopelagic:
Ch Life in the Oceans. Ocean Chemistry and Marine Life Ocean plants and animals remove and return many types of nutrients and gases to the water.
Plankton
Epipelagic & Deep Ocean. Pelagic Ocean Zones (open ocean) Epipelagic- 0 to 200m (photic zone) Epipelagic- 0 to 200m (photic zone) Mesopelagic- 200 to.
Plankton
Organisms Distribution Environment
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Chapter 15. Salinity Chemical weathering on land creates chemicals picked up by freshwater and delivered to the ocean Mainly sodium chloride Chemicals.
Chapter 15 Lecture Slides
Aliens on our planet Alexa Romersa. What are they? Are they rare? Do they live so far away that we would never find them? Are they dangerous?
Chapter 15 Life Near the Surface Copyright © 2016 McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written.
Marine Life.
Plankton Marine life is classified into three groups: Plankton, Nekton, and Benthos Plankton: the drifters Nekton: the active swimmers.
Chapter 15 Life Near the Surface.
Class The Oceans ADAPTATIONS TO LIFE IN SEAWATER
The Ocean Depths.
Chapter 17 sec3 Marine Ecosystems
Chapter 9 Marine Ecology.
Biotic and Abiotic Factors of the Ocean
15.1 The Composition of Seawater
Module 13 The Epipelagic Zone - Part 2 March 21, 2013
OCEAN WATER AND OCEAN LIFE
Projected changes to the tropical Pacific Ocean
Projected changes to the tropical Pacific Ocean
Ocean Water Earth Science Ch. 15.
Chapter 15 Life Near the Surface.
Oceans.
Midwater/Deep Ocean.
Plankton and Plankton Communities
Oceanic Zones Notes.
OCEANIC LIFE ZONES.
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Plankton!!! * Plankton don’t have eyebrows 01/17/13
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Aquatic Biodiversity Ch. 6, Part 1.
Planktonville Design the perfect plankton, and write about your Plankton and how it is best adapted for survivability in the ocean. Assignment is Due on.
OCEANIC LIFE ZONES.
Test #2 Results by Next Week
AP Biology Summer Workshop July 10th – July 14th
Projected changes to the tropical Pacific Ocean
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Projected changes to the tropical Pacific Ocean
The Discovery of Ocean Life
OCEAN WATER & OCEAN LIFE
Nutrient Cycles in Marine Ecosystems Part I
An Introduction to Ecology and the Biosphere
Presentation transcript:

The Open Ocean AKA EPIPELAGIC

OPEN OCEAN / EPIPELAGIC ZONE From surface to 100-200 m (300-600 ft) Beyond shelf break Similar to photic zone – layer from surface to the depth where light limits photosynthesis Phytoplankton main primary producers (where nutrients are available) Copepods most abundant zooplankton Almost all nekton carnivorous predators

ABIOTIC FACTORS Light Limited nutrients Organic particles sink before they can be released by bacteria, surface waters poor in nutrients, phytoplankton growth nutrient-limited Nitrogen limiting nutrient in ocean Iron limiting in Southern & equatorial Pacific oceans At high latitudes winter overturn & mixing bring nutrient-rich deep water to surface

BIOTIC FACTORS Staying afloat Finding food and avoid being eaten Cells & tissues denser than water Shells & skeletons more dense Finding food and avoid being eaten

ADAPTATIONS Staying afloat Increased water resistance to sink slower More surface area, more drag, slower sinking Increase buoyancy Storing lipids, gas-filled floats/swim bladders

ADAPTATIONS Finding food and avoid being eaten highly developed sense organs Vision – well developed eyes Lateral line – sense vibrations in the water Hearing Echolocation – built in SONAR in cetaceans Coloration & camouflage Countershading (dark top & light bottom) Excellent swimmers Streamlined Well-developed & efficient muscles High, narrow tails