Major roles in carbon source/sink dynamics both over Earth's history and in the present
Plant reproductive anatomy evolution in the lineage leading to gymnosperms
Innovations that took place
Seeds and pollen
Critical steps in plant evolution
Geologic changes
Favored gymnosperms over seed-free plants during the time of the dinosaurs
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Embryophytes (Land Plants)
Nonvascular plants (bryophytes)
Vascular plants (seedless)
Seed plants
After land plants took off, there was another bump in O2 levels by 1-2 orders of magnitude
Rise in O2 levels due to photosynthesis
CO2 is being fixed
Plants in the Carboniferous Period
Lycophyte trees
Horsetail
Fern
Plants in the Carboniferous Period
The first time plants get TALL!
Carbon dioxide sinks expanded by plants in the Carboniferous Period
1. Root acids weather continental rock, releasing calcium and magnesium that react with CO2 to form minerals
2. Boggy, waterlogged, anoxic soils lead to slow, incomplete decay of dead trees to become peat, which is converted to coal over millions of years
Lower CO2 levels
Big drop in global temperature
The Carboniferous Period led to a long, extended period with polar ice caps - an "Icehouse Earth" Period
Azolla
Common names: fairy moss, mosquito fern, water fern
Aquatic and very reduced in form compared to other ferns
Forms a symbiotic association with nitrogen-fixing cyanobacteria that it makes a home for within pouches in its leaves
Azolla use in organic rice farming in Southeast and South Asia
Ducks eat weeds and insects and Azolla
Azolla fixes nitrogen
Duck poop and dead Azolla fertilize soil
Higher rice yields with no chemical input
Azolla
Doubles its biomass in 1.9 days, faster than some bacteria
About 50 mya in the middle Eocene, the continents were clumped such that the Arctic ocean was enclosed and cut off from broader currents, leading to a thin freshwater layer over this ocean that huge mats of Azolla covered
Dead Azolla mats accumulated as stagnant sediment for ~800,000 years, drawing 80% of CO2 out of atmosphere and sinking it to ocean floor, becoming Alaskan oil deposits
"Seed-free" plants have been responsible for starting TWO "Icehouse Earth" periods by creating new mineral or organic carbon sinks, with lots of biomass and environmental conditions unfavorable for decay being critical to both events. We've been burning up those fossil fuel sinks as well as peat and rapidly heating our atmosphere today.
Gymnosperms
gymnos = "naked", sperms = "seed"
Only ~1000 species today, but much more diverse in the past
Include gnetophytes, cycads, gingko, and (mostly) conifers
Seed plants do not rise initially, have to wait until favored ~250-280 mya when there was a big change in climate in their favor that "drained the swamp"
Heyday in the Jurassic, and still dominate certain biomes like boreal forests (taiga) and alpine forests
Gymnosperm types
Gnetophytes
Cycads
Gingko
Conifers
Gymnosperm trees
Tallest Trees: Coast Redwood
Biggest Trees: Giant Sequoia
Oldest Trees: Bristlecone Pine
Rise of the seed plants
1. After the Carboniferous, seed plants come to dominate the landscape
2. Rise comes ~250-280 mya when there was a big change in climate in their favor that "drained the swamp" - formation of Pangea and uplift -> more arid land area
Pollen
Solution to Problem 4 of Adapting to Life on Land (Fertilization)
Cones
Gymnosperm reproductive structures
Anatomically akin to compressed fern fronds or lycophyte strobili, with scales that are modified leaves with sporangia (sporophylls)
Heterospory in gymnosperms
1. Megasporangia make megaspores that germinate to become the female gametophyte
2. Microsporangia make microspores that germinate to become the male gametophyte (pollen)
3. Each sporangium type is produced by a different type of cone (either on same or different tree)
4. Spores stay put in sporangia
Foot
Embryo
Archegonium
2 mm
Zygote
(2n)
(within archegonium)
Archegonia
Female
gametophyte
(n)
Protonemata
(n)
Rhizoid
Sporangium
Mature sporophytes
Capsule (LM)
Female gametophytes
Young sporophyte
(2n)
Reminder: only one type of spore in seed-free plant life cycles
Ovule
Mature sporophyte
(2n)
Ovulate cone
Integument
Pollen cone
Microsporocytes
(2n)
MEIOSIS
Microsporangia
Seedling
Megasporocyte (2n)
Megasporangium
(2n)
Germinating pollen grain
Microsporangium (2n)
Surviving megaspore (n)
Archegonium
Female gametophyte
Seeds
Food reserves
Seed coat (2n)
Sperm nucleus (n)
Pollen tube
Egg nucleus (n)
Haploid (n)
Diploid (2n)
Embryo (new sporophyte)
(2n)
Pollen grains (n)
MEIOSIS
FERTILIZATION
What's in a cone? Depends which cone
Pollen cone
Microsporocytes
(2n)
Pollen grains (n)
MEIOSIS
Microsporangia
Mature sporophyte
(2n)
Microsporangium (2n)
Previously: A sporophyte (2n) makes sporophylls (2n) that hold sporangia (2n) that make spores (n) by meiosis, which disperse and germinate to develop into gametophytes (n)
Adapted: The sporophyte (2n) makes pollen cones made up of sporophylls (scales, 2n) that hold microsporangia (2n) make microspores (n) by meiosis that germinate to develop into pollen grains (n)
Key Innovation #1
Microspores not dispersed
Key Innovation #2
Free-living male gametophyte moves by wind not water! (Solves Problem 4 of Life on Land - Fertilization)
Pollen is encased in sporopollenin. Has undergone 2 cell divisions. No more motile sperm and no antheridia.
Ovulate cone
Integument
Microsporocytes
(2n)
MEIOSIS
Microsporangia
Seedling
Megasporocyte (2n)
Megasporangium
(2n)
Germinating pollen grain
Microsporangium (2n)
Surviving megaspore (n)
Archegonium
Female gametophyte
Seeds
Food reserves
Seed coat (2n)
Sperm nucleus (n)
Pollen tube
Embryo
(2n)
Pollen grains (n)
MEIOSIS
FERTILIZATION
Immature ovulate cone
Integument (2n)
Megaspore (n)
Spore wall
Megasporangium
(2n)
Pollen grain (n)
Ovule = megasporangium surrounded by the protective structure that will become the seed coat (the integument)