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Tidal Forces01:06

Tidal Forces

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The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to...
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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.
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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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Membrane Fluidity01:23

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Cell membranes are composed of phospholipids, proteins, and carbohydrates loosely attached to one another through chemical interactions. Molecules are generally able to move about in the plane of the membrane, giving the membrane its flexible nature called fluidity. Two other features of the membrane contribute to membrane fluidity: the chemical structure of the phospholipids and the presence of cholesterol in the membrane.
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Tonicity in Plants00:53

Tonicity in Plants

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Tonicity describes the capacity of a cell to lose or gain water. It depends on the quantity of solute that does not penetrate the membrane. Tonicity delimits the magnitude and direction of osmosis and results in three possible scenarios that alter the volume of a cell: hypertonicity, hypotonicity, and isotonicity. Due to differences in structure and physiology, tonicity of plant cells is different from that of animal cells in some scenarios.
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Tonicity in Plants01:20

Tonicity in Plants

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Plant cells maintain appropriate osmotic balance in extreme conditions. For instance, plants in dry environments store water in vacuoles, limit the opening of their stoma, and have thick, waxy cuticles to prevent unnecessary water loss. Some species of plants that live in salty environments store salt in their roots. As a result, water osmosis occurs in the root from the surrounding soil.
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Related Experiment Video

Updated: Nov 27, 2025

Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
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Weak tides during Cryogenian glaciations.

J A Mattias Green1, Hannah S Davies2,3, Joao C Duarte2,3,4

  • 1School of Ocean Sciences, Bangor University, Menai Bridge, UK. m.green@bangor.ac.uk.

Nature Communications
|December 5, 2020
PubMed
Summary

During Snowball Earth glaciations, Cryogenian oceans had significantly weaker tides, potentially contributing to prolonged ice ages. This finding also offers insights into lunar evolution.

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Area of Science:

  • Paleoclimatology
  • Earth Science
  • Oceanography

Background:

  • The Cryogenian period (720-635 million years ago) experienced severe "Snowball Earth" glaciations.
  • These glaciations coincided with major supercontinent reorganization.
  • Contrasting predictions exist regarding ocean tidal energy during this period.

Purpose of the Study:

  • To investigate tidal amplitudes and energy dissipation in the Cryogenian ocean during Snowball Earth events.
  • To assess the role of tidal processes in the duration of these glaciations.
  • To constrain lunar distance and orbital evolution.

Main Methods:

  • Utilized an established numerical global tidal model.
  • Incorporated paleogeographic reconstructions of the Cryogenian period.
  • Simulated ocean tidal dynamics under Snowball Earth conditions.

Main Results:

  • Cryogenian oceans exhibited significantly diminished tidal amplitudes, 10-50% of present-day rates.
  • Associated tidal energy dissipation rates were also substantially reduced.
  • Weak tides suggest a potential contributing factor to prolonged glaciations.

Conclusions:

  • Near-absence of tidal processes may have prolonged Snowball Earth glaciations.
  • Results provide constraints on lunar distance and orbital evolution during the Cryogenian.
  • Future ocean simulations should incorporate explicit tidally driven mixing.