SYMBIOTIC ENVIRONMENT Flashcards

1
Q

WHAT IS SYMBIOSIS?

A

used to describe any permanent or long-
lasting association between two or more different species of
organisms.

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2
Q

HOST

A

-Refers to the larger member of the
symbiosis.
-Typically provides shelter for its
symbiont.

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3
Q

SYMBIONT

A

-Known as the smaller member in the
symbiosis.
- aid in supplementing nutrients that
the host can’t obtain sufficient
amounts .

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4
Q

CHARACTERISTICS OF ALGAL/INVERTEBRATE SYMBIOSES

A

High Genetic Diversity
Obligated symbiosis
Algae species can be extracellular or intracellular in their hosts.
Symbiosis’ specificity should be high
Algae is able to resist defensive mechanism of the
hosts

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5
Q

METABOLIC INTERACTIONS IN ALGAL/INVERTEBRATE SYMBIOSES

A

Algae Photosynthesis & Carbon Fixation
Nutrient Supply Absorption
Enhancement of Calcification
Shading Mechanism Developed by the Algae
Protecting Algae form Herbivores

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6
Q

The accumulation of calcium salts into body tissue, such as bones,
shells, and carapaces of the organisms.

A

CALCIFICATION

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7
Q

What is Coral Calcification?

A

A process by which corals produce calcium carbonate (CaCO3).
It is a measure of coral growth, which is important for healthy
reef ecosystems.

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8
Q

WHERE DOES CORAL CALCIFICATION OCCURS?

A

in the space between the innermost tissue of the corals, calicodermis, and the skeleton.

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9
Q

Calcification is accelerated by light

A

photosynthesis-driven process

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10
Q

CORAL CALCIFICATION EQUATION

A

Ca2+ + 2HCO3- -> CaCO3 + CO2 + H2O

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11
Q

WHY DO CORALS CALCIFY?

A

INCREASE SURFACE AREA
STRUCTURAL SUPPORT FOR THE ORGANISMS
A MECHANISM TO MAINTAIN ELEVATION ABOVE SEDIMENT-WATER INTERFACE.
A WAY OF MAINTAINING A CLOSE PROXIMITY TO HIGH LIGHT LEVEL
MEANS FOR KEEPING UP WITH SEA LEVEL RISE

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12
Q

WHAT ARE THE TWO SETS OF TISSUE LAYERS IN CORALS?

A

an oral diploblastic layer in which the epithelial layer does not calcify (dark pink).
aboral diploblastic tissue layer in which the epithelium calcifies (known as the calicodermis: darker red).

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13
Q

PROCESS ON HOW CORALS BUILD THEIR SKELETONS

A

-WATER EXCHANGE BETWEEN AMBIENT SEAWATER AND GASTROVASCULAR CAVITY (GVC) THROUGH THE POLYP MOUTH
-ACTIVE, PASSIVE OR PARACELLULAR FLUX FROM SEAWATER ACROSS TISSUE LAYERS INTO THE GVC
-EXCHANGE OF METABOLITES FROM RESPIRATION, PHOTOSYNTHESIS, AND OTHER METABOLIC PROCESSES BETWEEN GVC AND SURROUNDING GASTRODERMAL CELLS
- EXCHANGE OF IONS BETWEEN GVC, CALICODERMIS AND SITES OF CALCIFICATION BY PHAGOCYTOSIS, PHAGOSOME MIGRATION, ACTIVE/PASSIVE TRANSPORT MECHANISM

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14
Q

How does ocean acidification affect coral calcification?

A

Ocean acidification can negatively affect marine life, causing organisms’ shells and skeletons made from calcium carbonate to dissolve. The more acidic the ocean, the faster the shells dissolve.

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15
Q

What is phosphorus?

A

Phosphorus, like nitrogen, is a critical nutrient required for all life.

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16
Q

The most common form of phosphorus used by biological
organisms is phosphate (PO4).

A

formation of DNA

cellular energy

cell membranes

17
Q

What is Phosphorus Cycle?

A

refers to the movement of phosphorus within and between the
biosphere, hydrosphere, and geosphere.