L13- Cretaceous Terrestrial Ecosystems

The Cretaceous World-

  • continents still splitting apart, high sea levels, greenhouse world, shallow continental seas

  • CO2 still high but gradually declining to modern levels (icehouse world now), O2 gradually rising

  • climatically sensitive fossils→ difficult to interpret when continents are separate, no current between australia and antarctica, cool temperate at poles, latitudinal banding but gets dragged around by currents

Plants:

  • Early Cretaceous→ no angiosperms

    • bryophytes

    • lycopsids, ferns, sphenopsids→ fern prairies, all shrubs (undergrowth)

    • pteridosperms (bennettites and caytoniales) go extinct

    • cycads

    • gingkos

    • conifers→ all groups

    • gnetales appear→ last of sea plants (potential ancestor of angiosperm)

    → plants resemble the jurassic world

  • angiosperms appear→

    • first ones were small shrubs→ dark and disturbed hypothesis

    • pollen are found at equatorial latitudes→ originally at the equator, diversify north and south

      • can trace migration of angiosperms through their pollen grains and megafossil evidence

    • phylogeny of modern angiosperms→ are sister group to gynosperms (seed plants)

    • most present day angiosperms are tropical in their requirements:

      • 50% are confined to tropical regions

      • 75% have optimal development in tropical environments

        → modern angiosperm biota adds more evidence to the fact that it was tropical in origin

  • biomes→

    • the most diversity is in the angiosperm biotas e.g. tropical summerwet:

    • get polar forests→ evidence around northern and southern ice sheets

Insects:

  • there are at least 25 major Cretaceous deposits

  • diversification of insects is associated with angiosperm diversification, but insects did not drive the origin of angiosperms→ insects and plants are associated

  • the more diverse an angiosperm assemblage is, the more diverse insect assemblages are e.g. in the tropics

  • all three major groups of insects evolved advanced sociality (ants-bees-vespid wasps, termites and aphids)

  • get first amber deposits

  • crabs appear but are aquatic

Biotic Interactions:

  • first angiosperms are pollinated by pollen collecting or pollen eating insects

  • more derived angiosperms are pollinated by nectar later on

  • not much pollen and food dispersal at this time

  • plant-insect interactions can’t be linked to origin of angiosperms because these diversifications happened before

Fish:

  • new groups→ all modern groups of teleosts appear, huge diversification

  • there are still some basal actinopterygians

  • this is when fish become modern in aspect

Amphibians:

  • last of temnospondyls come through but disappear and are left with lissamphibians→ modern groups

Reptiles:

Synapsids:

  • only remaining synapsids are mammals→ diversify widely throughout jurassic-cretaceous but are not dominant in the biota (dinosaurs still dominating)

Anapsids:

  • only remaining groups are turtles→ debate if they are anapsids or not

Diapsids:

  • huge radiation of modern groups of snakes and lizards

  • ichthyosaurs and plesiosaurs persist in the shallow continental seas

  • crocodiles persist→ huge diversity

  • pterosaurs persist in the sky

  • dinosaurs continue to persist and dominate

  • taxonomy of dinosaurs

    • get two new groups→ get complete phylogeny of dinosaurs now

      • pachycephalosurs→

      • ceratopsids→

  • diet changes in the cretaceous→

    • mesophtyic diet changes to a cenophytic diet due to angisoperm diversifciation

    • no grass→ understory is ferns, lycopsids and horsetails, some dycots, dominated by fern priaries

Birds:

  • get ancient groups, diversify

  • birds evolved but lost ability to fly due to pterosaurs dominating

  • mass extinction wipes out most of the old groups→ birds diversify in pterosaur niche

  • there were flying birds that coexist with pterosaurs but there are much less of them→ found in china deposits

K/T Mass Extinction:

  • 5th mass extinction

  • dinosaurs disappear on the land, ammonites disappear in the oceans

  • boundary layer has high iridium layers, globally and at high and low sedimentation rates→ only from outer space

    • bolide hit planet

    • hit at the chixulub site→ can learn about the nature of the impact, material gets thinner away from this site

    • lots of basalt released from earth cracking open- outgassing, blocks out sunlight, no photosynthesising in the ocean, plants can’t grow back on land, nuclear winter, shut down of primary productivity→ increased extinction but bolide impact was the main cause

  • find layers of charcoal→ fires

  • finds layers of ferns→ grow back after fires

  • is the shortest mass extinction→ impact, aftereffects (earthquakes, tsunamis)

  • forest reestablish, survivor animals e.g. crocodiles, birds, repopulate planet