Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Experiment Videos

Hypersea and the land ecosystem

M A McMenamin1, D L McMenamin

  • 1Department of Geography and Geology, Mount Holyoke College, South Hadley, MA 01075-1484.

Bio Systems
|January 1, 1993
PubMed
Summary
This summary is machine-generated.

Related Concept Videos

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Paleoecological feedback and the Vendian-Cambrian transition.

Trends in ecology & evolution·2011
Same author

Ediacaran biota from Sonora, Mexico.

Proceedings of the National Academy of Sciences of the United States of America·1996
Same author

Late cretaceous atmospheric oxygen.

Science (New York, N.Y.)·1987
See all related articles

Land ecosystems exhibit higher productivity and diversity than marine ecosystems due to

Area of Science:

  • Ecology
  • Biogeochemistry
  • Evolutionary Biology

Background:

  • Land ecosystems surpass marine ecosystems in primary productivity and species diversity per unit area.
  • Eukaryotic life actively manages nutrient-rich fluid flow on land, influencing geochemical cycles.
  • This directed fluid flow and associated organisms are termed 'Hypersea'.

Purpose of the Study:

  • To introduce and define the concept of 'Hypersea' as a biogeophysical entity.
  • To explain the high productivity and diversity of terrestrial ecosystems compared to marine ones.
  • To elucidate the origins of coal deposits and the long-term dominance of land biota.

Main Methods:

  • Paleontological analysis of Lower Devonian fossils (Rhynie Chert).
  • Conceptual framework development for 'Hypersea' and 'hypermarine upwelling'.

Related Experiment Videos

  • Comparative analysis of land and marine ecosystem productivity and diversity over geological timescales.
  • Main Results:

    • Identified fossil evidence of Hypersea interactions in the Lower Devonian (approx. 400 million years ago).
    • Proposed 'hypermarine upwelling' as a mechanism driving coal formation.
    • Established Hypersea as a key factor in the long-standing ecological dominance of land biota.

    Conclusions:

    • Hypersea, a novel biogeophysical entity, explains the superior productivity and diversity of land ecosystems.
    • The concept of hypermarine upwelling provides insights into coal genesis and terrestrial ecosystem evolution.
    • Eukaryotic fluid management on land has had profound evolutionary and geochemical impacts.