Jove
Visualize
Contact Us

Related Concept Videos

Diversity of Archaea III01:27

Diversity of Archaea III

109
Crenarchaeota, a prominent phylum of Archaea, is remarkable for its ability to thrive in extreme environments characterized by high temperatures and acidity. These microorganisms inhabit sulfuric hot springs, volcanic systems, and submarine hydrothermal vents, where temperatures often exceed 100°C. The unique adaptations of Crenarchaeota not only allow survival under such extreme conditions but also provide insights into the mechanisms of life in primordial Earth-like...
109
Global Climate Change01:50

Global Climate Change

25.0K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
25.0K
Diversity of Archaea IV01:29

Diversity of Archaea IV

151
Hyperthermophilic archaea are a group of extremophiles thriving at temperatures above 80°C, often in hydrothermal vents and volcanic soils where conditions surpass the boiling point of water. At such temperatures, proteins, membranes, and DNA in most organisms degrade, but hyperthermophiles have evolved remarkable adaptations to maintain stability and function.Unique Cellular FeaturesHyperthermophilic membranes are composed of a monolayer of biphytanyl tetraether lipids, which resist...
151
The Fossil Record02:56

The Fossil Record

26.2K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
26.2K
Diversity of Archaea I01:30

Diversity of Archaea I

150
Archaea, a domain of single-celled microorganisms, are classified into five major phyla based on genetic and biochemical characteristics: Euryarchaeota, Crenarchaeota, Thaumarchaeota, Korarchaeota, and Nanoarchaeota. Among these, the phylum Euryarchaeota is notable for its remarkable diversity in morphology, metabolism, and ecological adaptations.Morphological and Metabolic DiversityMembers of Euryarchaeota exhibit a variety of cellular shapes, including rods and cocci. Their metabolic pathways...
150
Diversity of Protists III01:27

Diversity of Protists III

264
Rhizaria are a diverse group of unicellular protists characterized by their threadlike cytoplasmic extensions known as pseudopodia. These structures aid in both locomotion and feeding, giving Rhizaria an amoeboid appearance. Their amoeboid morphology once led to taxonomic confusion, but molecular phylogenetics has clarified their evolutionary placement and emphasized their shared use of pseudopodia despite divergent lineages.This clade comprises diverse lineages such as Chlorarachniophyta,...
264

You might also read

Related Articles

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

Sort by
Same author

Author Correction: Northern Scandinavian mountains supported by a low-grade eclogitic crustal keel.

Nature communications·2025
Same author

Northern Scandinavian mountains supported by a low-grade eclogitic crustal keel.

Nature communications·2025
Same author

Crustal melting and continent uplift by mafic underplating at convergent boundaries.

Nature communications·2024
Same author

No mafic layer in 80 km thick Tibetan crust.

Nature communications·2021
Same author

Rotation, Strain, and Translation Sensors Performance Tests with Active Seismic Sources.

Sensors (Basel, Switzerland)·2021
Same author

Southern Africa crustal anisotropy reveals coupled crust-mantle evolution for over 2 billion years.

Nature communications·2019
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 Video

Updated: Oct 13, 2025

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

12.6K

Long-lived Paleoproterozoic eclogitic lower crust.

Sebastian Buntin1, Irina M Artemieva2,3,4, Alireza Malehmir5

  • 1Department of Earth Sciences, Uppsala University, Uppsala, Sweden. sebastian.buntin@geo.uu.se.

Nature Communications
|November 13, 2021
PubMed
Summary
This summary is machine-generated.

Eclogite, a dense metamorphic rock, was found to persist in the lower crust below the Moho in the Fennoscandian Shield. This finding challenges established models of crustal evolution and delamination.

More Related Videos

Isolation of Quartz Grains for Optically Stimulated Luminescence OSL Dating of Quaternary Sediments for Paleoenvironmental Research
09:41

Isolation of Quartz Grains for Optically Stimulated Luminescence OSL Dating of Quaternary Sediments for Paleoenvironmental Research

Published on: August 2, 2021

3.1K
Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

11.9K

Related Experiment Videos

Last Updated: Oct 13, 2025

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

12.6K
Isolation of Quartz Grains for Optically Stimulated Luminescence OSL Dating of Quaternary Sediments for Paleoenvironmental Research
09:41

Isolation of Quartz Grains for Optically Stimulated Luminescence OSL Dating of Quaternary Sediments for Paleoenvironmental Research

Published on: August 2, 2021

3.1K
Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
09:45

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria

Published on: July 24, 2016

11.9K

Area of Science:

  • Geophysics
  • Petrology
  • Tectonics

Background:

  • The lower crust and crust-mantle boundary are critical to understanding Earth's structure.
  • Eclogitization of lower crustal rocks typically leads to delamination, a process not observed in this study.

Purpose of the Study:

  • To investigate the long-term stability of lower crustal eclogite.
  • To challenge conventional models of lithosphere evolution and cratonic crust stability.

Main Methods:

  • Acquisition and analysis of new wide-angle seismic data from the Paleoproterozoic Fennoscandian Shield.
  • Interpretation of seismic velocities and densities to infer rock composition and structure.

Main Results:

  • Identification of a 6-8 km thick body with high seismic velocity (Vp ~ 8.5-8.6 km/s) and density (>3.4 g/cm³).
  • This body lies beneath a thinned, high-velocity (Vp ~ 7.3-7.4 km/s) lowermost crustal layer extending over >350 km.
  • Evidence suggests partial transformation (50-70%) of mafic lower crust into eclogite during Paleoproterozoic orogeny without subsequent delamination.

Conclusions:

  • The study provides evidence for the long-term presence of lower crustal eclogite beneath the seismic Moho.
  • Findings challenge the expected role of eclogitization and delamination in lithosphere evolution and cratonic crust stability.