BI303: Chapter 1

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148 Terms

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How old is the Earth?

4.6 billion years old

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Prokaryote

A unicellular organism that lacks a nucleus and membrane-bound organelles

- no nucleus

- no membrane-bound nucleus

<p>A unicellular organism that lacks a nucleus and membrane-bound organelles</p><p>- no nucleus</p><p>- no membrane-bound nucleus</p>
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What are some examples of prokaryotes?

Bacteria and Archaea

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Eukaryotes

organisms made up of one or more cells that have a nucleus and membrane-bound organelles

- nucleus

- membrane-bound organelles

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Name parts of a cell that developed with eukaryotic development?

- nuclear membrane

- Peroxisome

- Lysosome

- ER

- name more!

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What are examples of Eukaryotes?

plants, animals, fungi, protists

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What is the oldest evidence of prokaryotic cells?

3.5 bya in Africa found in a pillow of lava that formed on the seabed

(3.6 - 3.8 bya trace fossils of prokaryotes)

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When did eukaryotic cells originate and how?

Around 2 - 2.5 bya; prokaryotes took in mitochondria and became the first eukaryotic cell

(2.7 bya - fossils proposed to be Eukaryotes)

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What is endosymbiosis

symbiosis in which one of the symbiotic organisms lives inside the other. (explains the origin of chloroplasts and mitochondria)

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Metazoans

multicellular animals

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Origin of Metazoans

875-650 mya; fossils found in Newfoundland (635-541 mya)

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What are some theories of how life originated?

- Primordial Soup

- Hydrothermal vents

- Meteors and Comets

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Primordial Soup

theory that the early oceans were a solution of organic molecules (that led to the development of living organisms)

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Metazoans are

monophyletic

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What are Metazoans numerous anamorphies?

- gastrulation and embryonic germ layer formation

- oogenesis and spermatogenesis

- unique sperm structure

- mitochondrial gene reduction

- epithelia with separate junctions

- tight junctions

- type IV collagen

- striate myofibrils

- actin and myosin

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anamorphy

new trait or character that has evolved in a species or group

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gastrulation

In animal development, a series of cell and tissue movements in which the blastula-stage embryo folds inward, producing a three-layered embryo, the gastrula. (major reorganization)

<p>In animal development, a series of cell and tissue movements in which the blastula-stage embryo folds inward, producing a three-layered embryo, the gastrula. (major reorganization)</p>
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oogenesis

the production, growth, and maturation of an egg, or ovum

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Spermatogenesis

the production of sperm cells

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epithilia

-tightly packed cells that cover body surfaces and line internal organs and cavities

-often functions as a barrier (skin)

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mitochondrial gene reduction

mitochondrial genes are transferred to the nucleus

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Why are mitochondrial genes only passed down from the mother?

The mitochondria comes from the egg, not the sperm (sperm's mitochondria are usually degraded and not incorporated into the developing embryo)

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Metazoa arose from

Opisthokonta

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Opisthokonta

the eukaryotic supergroup that contains

- fungi

- metazoa

- protists

- some plants

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Choanoflagellates

protists that are the closest living relatives of animals

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What are the 3 great domains?

Bacteria, Archaea and Eukaryotes

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Bacteria

- DNA dispersed throughout the cell

- no nuclei or membrane-bound organelles

- some use chlorophyll-based photosynthesis

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Archaea

- DNA dispersed throughout the cell

- no nuclei or membrane-bound organelles

- cannot use chlorophyll-based photosynthesis

- contains extremophiles (living in extreme environments)

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Chemoautotrophs

Organisms that use hydrogen sulfide or other chemicals as energy source instead of light.

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Halophiles

"salt-loving" archaea that live in environments that have very high salt concentrations

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Thermophiles

Archaea that thrive in very hot environments, such as volcanic springs.

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Acidophiles

grow best in acidic habitats

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Alkaliphiles

organisms that live above pH 8.5 (basic)

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Barophiles

can survive under extreme pressure and will rupture if exposed to normal atmospheric pressure

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How do Archaea differ from Bacteria and Eukaryota?

in the composition of their ribosomes, in the construction of their cell walls, and in the kinds of lipids in their cell membranes.

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Eukaryotes

- DNA is in membrane-bound nucleus

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Classification

The process of grouping things based on their similarities to sort evolutionary relationships

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Name the different percentages of groups of species described

- Arthropoda: 82%

- Molluscs: 5%

- Pladyhelminthes (flatworms - 1%?)

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Protists are

paraphyletic (not including all descendants of a common ancestor)

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Monophyletic

ALL descendants came from one common ancestor

<p>ALL descendants came from one common ancestor</p>
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Name an example of monophyletic groups

Mammals, birds, tetrapods and amniotes (reptiles, birds and mammals)

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Paraphyletic

pertaining to a grouping of species that consists of an ancestral species and some, but not all, of its descendants.

<p>pertaining to a grouping of species that consists of an ancestral species and some, but not all, of its descendants.</p>
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Name an example of a paraphyletic group

Crustaceans (bcs of hexapods - insects aren't included); invertebrates; reptiles

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Name the different databases used for species

- US Geological Survey (USGS) and ITIS (species name and classification)

- Catalogue of Life (CoL)

- Encyclopedia of Life (EOL) project: species name AND ecological info

- WoRMs (World Register of Marine Species): goal of listing all described eukaryotic species, including their higher taxonomy.

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When was the first trace of Eukaryotic life?

first benthic algae = 1.6 to 1.8 bya; first certain eukaryotic fossils of phytoplankton = 1.2 bya

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Geological Time Scale

- Paleozoic

- Mesozoic

- Cenozoic

<p>- Paleozoic</p><p>- Mesozoic</p><p>- Cenozoic</p>
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Precambrian (4.6 bya - 541 mya)

(Proterozoic Eon)

the oldest and longest span of geologic time; dominated by simple life forms like bacteria, algae and first multicellular organisms

- 3 "Snowball Earth" Events occurred at the end of the Proterozoic Eon

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What were the Snowball Earth Events caused by?

- extreme glaciation, covering things in ice

- reduction in greenhouse gases (less volcanic emissions)

(escaped the ice age through rapid warming and volcanic activity)

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These changes occurred during the breakup of supercontinent Rodinia,

the continent after Pangea

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Ediacaran Period (part of Precambrian; 635-541 mya)

First large, complex multicellular life appears (soft-bodied organisms); marks the transition of the explosion of life in the Cambrian Period

*Extinction of many soft-bodied creatures due to increased Oxygen in waters (ocean chemistry, ecosystem shift, or early predation could have played a role)

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What phyla were formed in the Ediacaran Period?

- Porifera

- Cnidaria

- Mollusca

- Annelida

and others (possibly Onychophora, Arthropoda, Echinodermata)

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Paleozoic Era (541 mya - 251.9 mya)

Begins with the Cambrian Explosion; earliest invertebrates, fish and amphibians arise (explosion of bilateria, seed ferns, gymnosperms)

*Ends with the permian mass extinction

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What phyla or characteristics arose in the Paleozoic Era?

- Large, calcareous body skeletons (archaeocyathans:coral like organisms that may have been early sponges)

- molluscs

- bryozoans

- brachiopods

- crustaceans

- chaetognaths

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What fossil defines the base of the Cambrian?

Treptichnus pedum; first penetrative animal that burrows, suggesting good use of bioturbation

<p>Treptichnus pedum; first penetrative animal that burrows, suggesting good use of bioturbation</p>
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Mesozoic Era (252-66mya)

Divided into three periods: Triassic, Jurassic, Cretaceous

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Triassic Period

Part of the Mesozoic Era, the period when dinosaurs first appeared. (248-213 million years ago)

- emergence of dinos

- warm climate

- Pangea

- vertebrate diversity

- end of the triassic: global extinction due to volcanoes and elevated CO2

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Jurassic Period

A period when enormous, herbivorous Dinosaurs began to develop

- first birds

- climate continues to be warm (stable climate)

- Pangea splits into two (forming tethy's sea)

- gymnosperms and advanced angiosperms appear

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What do we know about invertebrates during Jurassic?

Insects were leaf-miners = vegetation were vascular plants (more terrestrial plants cs of xylem and phloem)

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What is the name of the two landmasses that Pangea split into?

Gondowana and Laurasia

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What formed in between Gondowana and Laurasia

Tethy's Sea

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Why is the Tethy's Sea important?

- became home to marine invertebrates

- modern corals began to appear

- it was shallow, tropical and warm

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Cretaceous Period

- large scale fragmentation of Gondowana and Laurasia: forming Atlantic and Southern Oceans

- climate cools

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What marked the end of the Cretaceous Period?

the Cretaceous-Paleocene mass extinction caused by floods and volcanism and major meteors

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Cenozoic Era (66 Mya - present)

"Age of Mammals"

- worlwide cooling trend

- continents began taking their current locations

Current Extinction

- habitat loss

- introduced species

- pollution/toxins

- overexploitation

- climate change

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71% of the Earth's surface is covered in

salt water

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How much of Earth's inhabitants live in the ocean?

99%

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Of the 31 living animal phyla, 13 are marine:

- Placozoa

- Ctnetophora

- Chaetognatha

- Dicymedia

- Cycliophora

- Gnathostomulida

- Phoronida

-Brachiopoda

-Kinorhyncha

-Priapula

-Loricifera

-Echinodermata

-Hemichordata

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What is the total productivity of seas?

48.7 x 10^9 metric tons of carbon per year

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Average salinity of seawater

3.5%

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Why are marine environments a suitable place to live for marine organisms?

- Stable temperatures; water has high heat capacity

- Stable pH

- Nutrient availability

- Water provides buoyancy (reduces the effects of gravity)

- Salinity works well with marine organisms and their osmotic pressure (less stress on their bodies)

-

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Oxygen minimum zones (OMZ)

Hypoxic regions of ocean sandwiched between upper and lower oxygenated layers

commonly found in deep-sea ecosystems

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Littoral zone

shoreline

<p>shoreline</p>
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supralittoral zone

"splash" zone; rarely covered with water

<p>"splash" zone; rarely covered with water</p>
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Eulittoral zone

The area between high tide and low tide. Organisms here must be adapted to live in wet and dry environments; intertidal zone

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Sublittoral zone

the ocean zone that begins at the low-tide limit and stretches to the edge of the continental shelf; never uncovered with water

<p>the ocean zone that begins at the low-tide limit and stretches to the edge of the continental shelf; never uncovered with water</p>
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Continental shelf

part of a continent that extends out underneath the ocean; avg. depth 150-200 m

<p>part of a continent that extends out underneath the ocean; avg. depth 150-200 m</p>
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Continental edge

The point at which the continental shelf which surrounds each continent begins to angle sharply downward

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Abyssal plain

a large, flat, almost level area of the deep-ocean basin;

contains seamounts, ridges and mountain ranges (avg. 4km below surface)

<p>a large, flat, almost level area of the deep-ocean basin;</p><p>contains seamounts, ridges and mountain ranges (avg. 4km below surface)</p>
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Pelagic

open ocean

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Epipelagic zone

The lighted, or photic, zone in the ocean.

<p>The lighted, or photic, zone in the ocean.</p>
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Mesopelagic zone

The pelagic layer of the ocean where light can penetrate, yet without the intensity to support photosynthesis

<p>The pelagic layer of the ocean where light can penetrate, yet without the intensity to support photosynthesis</p>
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Bathypelagic zone

The pelagic environment from a depth of 1000 m to 4000 m. No sunlight at all.

<p>The pelagic environment from a depth of 1000 m to 4000 m. No sunlight at all.</p>
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Abyssopelagic zone

The pelagic environment from a depth of approximately 4000m to 6000 m. No sunlight at all.

<p>The pelagic environment from a depth of approximately 4000m to 6000 m. No sunlight at all.</p>
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Hadalpelagic zone

includes areas found in deep-sea trenches and canyons (6k meters and deeper)

<p>includes areas found in deep-sea trenches and canyons (6k meters and deeper)</p>
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Benthic

bottom of an aquatic ecosystem; consists of sand and sediment and supports its own community of organisms

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Demersal

organisms that live near the seafloor

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Benthic Boundary Layer (BBL)

the layer of water that sits on top of the bottom of a body of a water; sediment suspension (diversity increases near the bottom of the sea floor)

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Epifauna (epibenthic)

Animals that live on the surface of the substrate

ex.

- sea anemones

- sea sponges

- snails

- barnacles

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Infauna

animals that burrow in the substrate (large invertebrates)

ex.

- clams

- worms

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Interstital organisms

microscopic animals that live in the spaces between sand grains

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Meiofauna

organisms smaller than 0.5 mm (fall under interstitial organisms)

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Name the five phyla of metazoans that are meiofauna

Gastrotricha

Gnathostomulida

Kinorhyncha

Loricifera

Micrognathozoa

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Errant

motile and mobile benthic organisms (crabs and worms)

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Sessile

organism that does not move (remains in one place); ex. sponges and corals

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Sedentary

organisms weakly attached to their substrate (ex. crinoids, clams, anemones)

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Pelagic zone

The open-water component of aquatic biomes.

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neritic zone

area of ocean over continental slope

<p>area of ocean over continental slope</p>
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oceanic zone

vast open ocean from the edge of the continental shelf outward

<p>vast open ocean from the edge of the continental shelf outward</p>
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Photic Zone

Portion of the marine biome that is shallow enough for sunlight to penetrate.

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Aphotic zone

permanently dark layer of the oceans below the photic zone

consists of:

- disphotic

- twilight

- mesopelagic zone