User:Jtwsaddress42/Projects/Project 1/Chapters/Chapter 11

Phase I - The Rise of Neomurans and the Modern Aerobic Atmosphere (950-600 mya)

Neomuran Revolution (950 mya) - Loss of murein cell wall
Archaeabacteria (850 mya) - Methanogenesis/Extremophiles
Eukaryotes (850 mya) - Phagocytosis & Massive HGT, Endomembrane System, Endosymbiosis
- Protokaryotes
- Eokaryotes
- Orthokaryotes
- Neokaryotes
- Scotokaryotes & Coricates
Podiata
Opisthokonta
Snow Ball Earth Episodes
Modern Aerobic Atomsphere (600 mya)

From Neomura to Podiata

Loss of Cell Wall

Isoprenopid Ether Lipids^[j]

Archaebacteria

Phagocytosis^[k]

Cytopharynx & Ciliary Paraxonemal Rods

Euglenozoa

Ventral Feeding Groove

Eruptive Psuedopodia^[i]

Percolozoa^[a]

Dorsal Ciliary Vane

Eolouka^[b]

Ventral Ciliary Vane^[h]

Myosin Domain Fusions

	Neolouka^[c]

Anaerobes^[e]	Metamonada^[d]

Ciliary Gliding^[f]

Podiata

Podiates

Scotokaryotes

Cortical Alveoli

Chloroplast Endosymbiont

Plantae^[g]

Plantae Endosymbiont

	Hacrobia

	SAR supergroup

Chromista

Corticates

Neokaryotes

Orthokaryotes

Eokaryotes

Protokaryotes

Archaebacteria

Eozoa^[l]

Neozoa^[m]

Corticata

Neomura^[n]

0.9 GYA

From Podiata to Opisthokonta

Ciliary Gliding

Planomonadida^[o]

Psuedopods^[s]

	Mantamonas

	Diphylledia

CRuMs

Catenins^[q]

Broad Psuedopods

Amoebozoa

Narrow Psuedopods^[p]

Breviatea

	Apusomonadida

Anterior Cilium Lost	Opisthokonta

Obazoa

Unikonts^[r]

Varisulca^[t]

Amoebozoa

Obazoa

Podiata

From Opisthokonta to Metazoa

Cavalier-Smith describes the Opisthokonts as being comprised of Choanozoa, Metazoa, and Fungi.^[1] In this diagram Cavalier-Smith's Fungi equates to Holomycota and Fungi is used more restrictively. Cavalier-Smith's Choanozoa equates to all Holozoans except Animals (Metozoa). Here Choanozoa is used in a more conventional and restrictive manner.

Loss of Anterior Cilium

Tapering Psuedopods^[w]

Cristidiscoidea