Marattioid Ferns

Order Marattiales

The Marattiales are a group of ancient tree ferns that date back to the Carboniferous coal age . They are uncommon tree-ferns of the modern tropics with six living genera and 90 species. This group was very abundant and diverse in Paleozoic lowland swamps, even dominant at the end of the Carboniferous, before seed plants began to takeover dominance. A well-known marattialean fern of the Carboniferous is Psaronius which existed in the understory of lepidodendrid swamps.

Ecology & Form

Stems

    • Stump-like, unbranched rhizome that can attain tree stature

    • Dictyostele present in stem

Leaves

    • Large compound leaves (fronds)

    • Croziers or fiddle heads

Roots

    • Abundant adventitious roots that are large and fleshy

    • Completely encase the stem of plant

Reproduction

    • Spore-bearing with large sporangia

      • Eusporangiate: large sporangia with thick walls and 100s of spores

      • Sporangia fuse into a synangium borne abaxially on ultimate pinnule laminae

Geologic Range

Above: rhizome stump of Marattia

Above: Leaves of Marattia

Above: Sporangia of Angiopteris and Marattia

Diversity

  • 6 living genera (90 species): Angiopteris, Christensenia, Danaea, Eupodium, Marattia, and Ptisana

Stems

Psaronius

  • Abundant in the Pennsylvanian

  • Form taxon for the trunk, which may have been up to eight to ten meters in length

  • P. simplicicaulis (Dimichele & Phillips 1977)

    • One of the earliest marattialean ferns from the Early Pennsylvanian of North America

  • P. renaultii (Williamson 1876)

Leaves

  • The ferns possessed a large crown of pinnately-compound leaves inserted in spirals or vertical rows on the trunk

  • The fronds were large, up to three meters in length, bilaterally symmetrical, and planate

  • The petioles have a U-shaped vascular trace

Pecopteris

  • Devonian - Carboniferous, with the greatest diversity in the Pennsylvanian

  • Form genus for compressions of leaves of marattialean ferns during the Carboniferous

    • It is also the form genus for some true ferns (Polypodiidae) and a least one seed fern (Taylor et al. 2009)

  • There are over 250 species of Pecopteris named (Robertson & DiMichele 1997)

Scolecopteris

  • Watson 1906

  • Form genus for permineralized leaves

Caulopteris

  • Form genus for compression or impression petiole scars

Qasimia yunnanica

  • Fronds at least bipinnate. Pinnules taeniopteroid or

  • neuropteroid, bases cordate, apices rounded. Midvein distinct [and

  • straight]. Lateral veins curved, rising at an acute angle, perpendicular

  • or subperpendicular to pinnule margin. In vegetative pinnules, lateral

  • veins commonly bifurcate twice, occasionally three times, showing

  • first bifurcation near the midvein, with a vein density of 40–50 veins

  • per centimeter at the pinnulemargin. In fertile pinnules, lateral veins bifurcate

  • once nearmidvein,with vein density less than half of vegetative

  • pinnules. Fertile pinnules identical in size and shape to vegetative pinnules.

  • Synangia, as pendants, abaxially attached, [arranged in one row

  • on each side of midvein], born on every individual lateral vein branch,

  • closely spaced, with length of nearly half-width of pinnules, and in a

  • ‘louvered’ pattern [or an imbricate arrangement]. Each valve of

  • bivalvate synangia composed of elongated and laterally fused sporangia.

  • [Sporangial number per valve varyingwith synangiumlength, up to 40.]

  • Sporangia [long ellipsoid, exannulate, with length near synangium

Roots

  • Abundant roots that are large and fleshy, completely encasing the stem forming a root mantle

  • The root cross-section reveals an exarch actinostele

  • The roots that are closest to the stem have a thick, sclerenchymatous cortex, and reinforced the trunk which lacked secondary xylem

Reproduction

  • Spore-bearing

  • Fertile fronds bore synangia composed of eusporangia on the abaxial surface, commonly clustered near veins of ultimate pinnules

  • Sporangia have uniform dehiscence along the midline of the sporangia

  • Spore genera Punctatisporites and Laevigatosporites are associated with Pecopteris foliage

Above: Psaronius, an extinct Marattioid fern common in the Carboniferous Period

Below: a cross-section of Psaronius, showing the stem and root mantle


Additional Resources