Lecture 4 : The Transition to Land: From Green Algae to Vascular Plants

Overview of the Transition to Land

  • General Context: The transition of green plants to a terrestrial environment is a central theme in evolutionary biology. This movement involves the evolution of green algae into land plants.

  • Timeline: The first land plants appeared approximately 470470 MYA.

  • Green Plants Definition: Includes all organisms commonly known as green algae and land plants.

  • Land Plants (Embryophytes): This group includes mosses, lycopods, ferns, seed plants, and flowering plants.

  • Aquatic Ancestry: Green plants shifted from aquatic environments to land, with the process roughly beginning around 470470 MYA.

  • Evolutionary Lineage: All land plants evolved from a common ancestor belonging to the green algal group known as Charophyta.

Green Plants Going Terrestrial: Ancestry and Early Adaptations

  • Freshwater Ancestors: The ancestors of land plants were freshwater algae.

  • Charophytes: These are the closest relatives to land plants. While they largely live in water, many also inhabit wet rocks in moist environments and possess specific adaptations to drought.

  • Reproductive Structures (Chara):

    • Oogonium: The structure containing eggs.

    • Antheridium: The structure containing sperm.    

    • Zygote: The cell formed via fertilization between two gametes (2extn2 ext{n}). In Chara, the zygote is retained on the parent plant and protected by a special layer to prevent dehydration.

  • Early Paleozoic Charophytes: These fossils are rare. Two notable examples include

    • Parka: Features an upper and lower epidermis and sporangia where spores are formed. It is thought to be related to Coleochaete algae

    • Coleochaete algae: Often identified as the direct ancestors of land plants. They grow on wet rocks, and their spores are adapted for drier conditions.

The Benefits and Challenges of Coming Ashore

Plants moving from water to land faced significant environmental changes:

  • Benefits (Pros):

    • Increased Light: More light is available on land compared to underwater.

    • Resource Accessibility: Carbon dioxide (CO2CO_2) and minerals are more accessible.

    • Ecological Opportunity: Initially, there was less competition and a total absence of herbivores.

  • Challenges (Cons):

    • Staying Hydrated: High risk of drying out (desiccation).

    • Water Acquisition: Water is no longer available to every cell; it must be sourced from the substrate.

    • Structural Support: Loss of buoyancy provided by water necessitates internal mechanical support.

    • Fertilization: It is much more difficult for sperm to reach eggs without a continuous water medium.

    • Temperature Fluctuations: Terrestrial environments have a higher chance of overheating or rapid temperature changes.

Microfossil Evidence of Early Land Plants

  • Earliest Evidence: Starting from the Middle Ordovician (470470 MYA), microfossils provide the first evidence of structures for water transport, mechanical support, reproduction, and protection.

  • Microfossil Types:

    • Cryptospores: Spore-like microfossils found in lower Palaeozoic rocks. the word "crypto" means secret or hidden. They pre-date larger plant fossils and represent the first evidence of evolution from algal ancestors.

    • Tubes: Microscopic structures used for transport or support.

    • Cuticles without Stomata: Protective outer layers found in early fossils.

  • Sporangia with Cryptospores: Rare finds from the Middle Ordovician of Oman (Wellman, Osterloff & Mohiuddin, Nature 2003) confirm that the earliest cryptospores developed within sporangia (organs for spore production). The spore walls are comparable to those of liverworts.

  • Cryptospore Forms: Include tetrads (four spores), dyads (two spores), and monads (single spores).

Non-Vascular Land Plants: Bryophytes

  • Classification: Includes Liverworts, Hornworts, and Mosses.

  • Physical Characteristics:

    • Small stature.

    • Rhizoids: Thin structures extending from the lower epidermal cells. These are similar in structure and function to the root hairs of vascular land plants.

    • Lack of vascular tissue.

    • Veinless tissue.

    • Thin cuticles, often lacking stomata.

    • Plain spores.

  • Liverwort Cuticles: Evidence from the Middle Devonian shows liverwort cuticles without stomata, similar to extant liverworts.

Evolutionary Innovations and Vascular Land Plants

To be defined as a vascular land plant, an organism must meet three criteria:

  1. Vascular System: Serves for the transport of water, nutrients, and photosynthesis products, while providing mechanical strength.

  2. Cuticle with Stomata: Provides protection and allows for regulated gas exchange.

  3. Trilete Spores: Spores with a tough wall to prevent drying out and facilitate air transport.

Sequence of Appearance in the Fossil Record:

  • Step I: Dominance of bryophytes and other non-vascular plants (associated with cryptospores).

  • Step II: Increase in fragments of vascular plants, appearing slightly later in the record (associated with trilete spores).

Macrofossil Evidence and the "Gap"

  • The Fossil Gap: There is a significant gap of approximately 3838 million years between the first vascular plant microfossils (e.g., Ambitisporites) and the first macrofossil of a whole land plant (Cooksonia).

  • Order of Appearance in Fossil Record:

    • 1. Cooksonia

    • 2. Baragwanathia

    • 3. Aglaophyton

    • 4. Zosterophylls

    • 5. Euphyllophytes

Detailed Profiles of Early Land Plants (By Increasing Complexity)

  1. Aglaophyton: A protracheophyte (non-vascular land plant).

    1. No true vascular system, but possesses tiny tubes.

    2. Features sporangia at the tips of stems.

    3. Exhibits dichotomous branching.

    4. No real roots, but possesses rhizoids.

  2. Cooksonia:

    1. Simple vascular system.

    2. Dichotomous branching.

    3. Terminal sporangia.

    4. No real roots, only rhizoids.

    5. No leaves.

    6. Information is often derived from dissolved sediments; organic material is studied via electron microscope to identify trilete spores and cuticula.

  3. Zosterophyllum:

    1. More complex vascular system.

    2. Lateral sporangia (located on the side of the stem)

    3. Axes may have small spines.

    4. Includes rhizomes (underground stems), but still no real roots.

  4. Psilophyton (a Euphyllophyte):

    1. Central stem with fertile and sterile branches.

    2. Complex vascular system

    3. Terminal sporangia on fertile branches

    4. Possesses true roots

    5. Still no leaves.

  5. Baragwanathia:  

    1. An early lycopod

    2. Remarkably large for its time, with axes reaching up to 30cm30\,\text{cm}

    3. Highly significant: The only plant of its time to possess leaves and roots

    4. Small structures between the leaves are likely sporangia.

Relationships and Phylogeny

  • The Major Dichotomy: Progress in paleobotany shows that vascular plant phylogeny split into two major clades approximately 415415 million years ago (Late Silurian–Early Devonian):

  • Lycophytes: Developed leaves and roots earlier and independently from other plants.

  • Euphyllophytes: Includes all other vascular plants.

  • Common Early Plants Summary: Five key examples are Cooksonia, Aglaophyton, Zosterophyllum, Baragwanathia, and Psilophyton.