Biotic producers of Carbonate sediments

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What is a coelomate?

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A cavity that is filled with a fluid that contains organs.

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Sponges

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  • Most primitive animal

  • Cells are organized into a multicellular body and held together by a gelatinous substance, no tissues or organs

  • Fixosessile organisms

  • Filter feeders on detritus or microscopic organisms

  • produce toxins to avoid predation and protection

  • main modern reef builders

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64 Terms

1

What is a coelomate?

A cavity that is filled with a fluid that contains organs.

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2

Sponges

  • Most primitive animal

  • Cells are organized into a multicellular body and held together by a gelatinous substance, no tissues or organs

  • Fixosessile organisms

  • Filter feeders on detritus or microscopic organisms

  • produce toxins to avoid predation and protection

  • main modern reef builders

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3

What us the osculum of a sponge

  • The central cavity of a sponge

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4

Spicule

The hard skeleton of a sponge that is preserved in the rock record

  • Can be siliceous or calcareous

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Demosponge

  • Skeleton mainly composed of spongin

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Hyalosponge

  • Skeleton mainly composed of spicules

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Calcisponge

  • skeleton composed of calcium carbonate

  • Limited to shallow warm tropical areas

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8

Ecological characteristics of sponges

  • Can tolerate deep muddy water

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9

Archaeocyatha

  • Calcareous sponges with double walls from the Cambrian

  • First skeletal reef builders

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10

Stromatoporoids

  • Calcareous skeleton

  • Parallel lamellae

  • Intersected pillar

  • Most important reef builders in the late ordivician-devonian

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11

Whya re sponges so important in carbonate sedimentology?

-Spicules are dominant deep water shelf to slope deposits

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12

Bryozoans

  • coelomates

  • Colonial organisms

  • Bilateral symmetry

  • Lophophores

  • Reproductive organs

  • Circulatory and digestive system

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13

What is a lophophore

Used for filter feeding by organisms

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14

What kind of energy environments can bryozoans be found in?

  • Branching bryozoans in low energy lagoons

  • Fenestrate bryozoans in high energy reefs

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15

Bryozoans in the environment

  • Fixosessile, epifaunal and filter feeders

  • Act to trap loose sediment forming skeletal pavement

  • Reef builders,

  • No photosynthetic component so can tolerate deep turbic water salt fluctuations and high levels of sediment

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Why are bryozoans important in carbonate geology

  • Common in all environments

  • Form and shape tells us about the environment

  • Important reef builders in paleozoic rocks

  • Act as binders baffles and stabilizers

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17

Brachiopod morphology

  • Protostome

  • Plane of symmetry perpendicular to hinge line

  • Pedicle moves the brachipod around

  • lopophore

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18

Different Brachiopod life strategies

  • Fixosessile

  • Infaunal (burrowing)

  • Librosessile (free lying)

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19

Brachipod shell composition

  • Carbonate

  • multiple layers of sheet like calcite (foliated)

  • These layers are at a gentle angle

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20

Are molluscs or Brachiopods are dominant in modern day?

Molluscs, up to the outer slope

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21

Why are brachiopods important in carbonate sedimentology

  • Good biostratigraphic markers

  • usually well preserved even in altered limestone and preserved the original chemical signature of the water

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22

Protosome vs deuterosome

  1. Protosome is mouth forms before the anus

  2. Deuterddtome the anus forms before the mouth

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23

Overview of Phylum Echinodermata

  • Benthic (on the sea floor)

  • Vagile (move on sea floor)

  • Can swim against current

  • From Cambrian to present day

  • Invertebrates

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24

What kind of echinoderms are carnivores?

Starfish

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25

Ossicles

  • Calcareous endoskeleton of echinoderms

  • High Mg Calcite

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Echinoder, fossils sediment relationship

  • Crinoid grains for sediment

  • Reef destroyer (when the bore into them)

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Why are echinoderms important in carbonate geology?

  • Major contributor of carbonate sedimentd

  • Dont like hyper saline environments

  • Indicative of storm deposits

  • Open marine conditions

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28

Coral Overview

  • Cnidarians

  • No organs

  • Tissue level organiszation

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29

Symbiotic relationship with cnidarians and zooxanthellates

  • Dynophlagelates are friendly with cnidarians and allow corals to get quiet large in size

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Cnidarian life cycle

  • Polyp, asexually reproduce through budding and create haploid cells

  • Medusa: adult free swimming, jellyfish shaped that reproduces sexually

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Class Anthozoa is made up of:

  • Zoantharia

  • Tabulata

  • Rugosa

  • Scleractinia

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32

Subclass Zoantharia

Sea anemones and true corals, solitary or colonial and are entirely marine

  • Reef builders

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Order Tabulata

Colonian Calcitic skeleton in the paleozic, permian extinction

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Order Rugosa

Solitary or colonial, calcitic skeleton in the paleozoic (permian extinction)

  • Abundance of diversity in silurian and devonian

  • Paleozoic coral-stromatoporoid reef builders

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Order Scleractinia

  • SOlitary or colonial, aragonitic skeleton, modern day corals

  • Solitary lives in deep water

  • main modern day reef builders

  • Fixosessile

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Hermatypic vs ahermatypic corals

Hermatypic corals need to be in the photic zone

Ahermatypic corals dont need light

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Why are corals important in carbonate geology

  • Built large reefs in the phanerozoic

  • Need light, no turbidity, little nutrients

  • Significant sediment producers

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38

Foraminifers

  • Single Cell Eukaryotes

  • Construct a test

  • Most are marine,

  • Present everywhere from equator to the poles

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39

How are the single cell forams divided?

  • Granular endoplasm

  • Transparent Ectoplasm

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40

WHat are pseudopods used for?

  • Locomotion

  • Anchoring

  • Capturing food

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41

What do symbionts allow to happen for marine life?

  • More energy accumulation and therefore large size

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42

Why are forams important in carbonate geology

  • Major sediment producers (Caco3)

  • Good paleoenvironmental indicators

  • Individual species are happy in very specific environments

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43

Calcareous algae overview

  • Multicellular algae

  • Photosynthetic autotrophs

  • Calcified thalus

  • Green Algae

  • Red Algae

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44

Green Algae

  • tropical algae

  • Most common in backreef and lagoonal setting (low energy)

  • Shallow water

  • Important carbonate sediment producers

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45

Calcareous Red Algae

  • Red algae is very good at absorbing light

  • Can live in deep and cold water

  • Coralline algae is the only modern algae around

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Why is calcareous algae important for carbonate geology

  • Major sediment producers (and micrite)

  • Best paleoenvironment indicators

  • Water depth, photic zone, low nutrients, low turbidity, Greatly affected by temperature

  • Very important as reef builders, binders bafflers and framers

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47

Arthropod overview

  • Protosomes

  • Most diverse animal phylum

  • Underrepresented in rock record due to difficulty preserving

  • Open circulatory system, blood moves through the body

  • Exoskeleton

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Trilobite

  • 3 lobes

  • Oldest animal with advanced eyes (compound eyes)

  • Benthix, vagile and deposit feeders

  • Like murkey deep water

  • Cruziana trace fossil

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49

WHy are Trilobites important in carbonate geology

  • Went extinct at the permian

  • Occupy all geological niches

  • Not reef builders

  • Warm and cool water

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50

Ostracods

  • Marine and fresh water

  • Has 2 valves

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51

Why are ostacods not important in carbonate geology

  • Not abundant, lagoonal deposits

  • cant tell environmental from thin section only

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52

Molluscs overview

  • Protosome

  • Organs

  • Bilateral organism

  • Solitary

  • Open circulatory system with heart

  • Respiratory system

  • Digestive system with radula (teeth)

  • Nervous system with tentacles and eyes

  • foot for locomotion

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53

Bivalve

  • Muscle foot for locomotion and burrowing

  • Mantle secretes calcareous shell and forms siphons for filter feeding

  • Gills used for filter feeding

  • Symmetry is along hinge line

  • mainly aragonite shells, so no external structure

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54

What is Pectinid movement

  • Bivalves that live ithin the water column expell water to move around

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55

Name the 5 microphagy feeding strategies

Labial Palp deposit feeders

Epifaunal suspenion feeders

Infauanal non siphonate suspension feeders

Infaunal siphonate feeders

infaunal mucus tub feeders

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56

Class Cephalopods

  • Fast swimming through jet propulsion

  • Advanced nervous system

  • Shell devided into chambers with septa

  • Only Nautoloids are around currently

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4 different ammonitic suture patterns

  • Ammonitic suture (most recent)

  • Ceratitic suture (permian tri)

  • GOniatitic (devonian Carbonif)

  • Agoniatitic (oldest)

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Belemnites class

  • Thick guard of prismatic calcite

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Gastropod class

  • Large foot

  • Torsion during development

  • Entirely aragonitic (rarely preserved)

  • Benthic

  • Planktic

  • Epiplanktic

  • Nektic

  • Land dwelling

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Microphagy of Gastropods

  • Herbivores

  • Carnivores

  • Detritus feeders

  • Suspension feeders

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61

WHy are molluscs important for carbonate geology

  • Rudist bivalves built reef

  • Gastropods and bivalves can produce a lot of pecal pellets

  • Ammonites are good biostrat indicators

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