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Migration00:53

Migration

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Migration is long-range, seasonal movement from one region or habitat to another. This common strategy, carried out by many different organisms around the world, is an adaptive response that typically corresponds to changes in an organism’s environment, like resource availability or climate. Migrations can involve huge groups of thousands of animals as well as single individuals traveling alone and can range from thousands of kilometers to just a few hundred meters.
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Cell Migration01:09

Cell Migration

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Cell migration, the process by which cells move from one location to another, is essential for the proper development and viability of organisms throughout their life. When cells are not able to migrate properly to their ordained locations, various disorders may occur. For example, disruption in cell migration causes chronic inflammatory diseases such as arthritis.
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Cell Migration01:19

Cell Migration

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Cell migration is a process by which the cells move from one location to another, playing an essential role in embryological development, repair and regeneration, immune response, and metastasis. Cells migrate in response to chemical or mechanical signals generated by specific organs or tissues. The overall mechanism includes three steps - polarization, protrusion, and release. Polarization involves the formation of a distinct cell front and rear, which determines the direction of movement.
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Torque Free Motion01:15

Torque Free Motion

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The torque-free motion refers to the movement of a rigid body in space when no external torques are acting upon it. This type of motion can be observed in environments where there are no external forces or frictions, like in outer space. For example, a rotation of Mars in space is a torque-free motion. Mars is an axisymmetric object, meaning it has an axis of symmetry along which it rotates, designated as the z-axis. The rotating frame of reference is defined such that the center of mass of...
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Cell Motility through Blebbing01:16

Cell Motility through Blebbing

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Blebs are a type of membrane protrusion formed by the internal hydrostatic pressure of the cytoplasm. Blebs are observed in several cell types, including fibroblasts, immune cells, and single-celled organisms like the amoeba. The primary function of blebs is cell locomotion and apoptosis, but they are also found during necrosis and cell division. The life cycle of a bleb comprises an initiation phase followed by the expansion and retraction phases.
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Cancer Cell Migration through Invadopodia01:35

Cancer Cell Migration through Invadopodia

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Invadosome is a broad category of cell surface structures with proteolytic activity that  degrades the extracellular matrix (ECM). Invadosomes are present in normal cell types, including macrophages, endothelial cells, and neurons, as well as tumor cells. Although the macrophage podosomes and tumor cell invadopodia are classified as invadosomes, they have different structures, molecular pathways, and functions. Podosomes are short structures that last for a few minutes. However,...
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Related Experiment Video

Updated: Dec 2, 2025

Evaluation of Cancer Stem Cell Migration Using Compartmentalizing Microfluidic Devices and Live Cell Imaging
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Evaluation of Cancer Stem Cell Migration Using Compartmentalizing Microfluidic Devices and Live Cell Imaging

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Megaripple Migration on Mars.

S Silvestro1,2, M Chojnacki3,4, D A Vaz5

  • 1INAF Osservatorio Astronomico di Capodimonte Napoli Italy.

Journal of Geophysical Research. Planets
|November 2, 2020
PubMed
Summary
This summary is machine-generated.

Active Martian megaripples, including bright Transverse Aeolian Ridges (TARs), have been observed migrating. This indicates these features are not relics of past climates but are active today, driven by Martian winds.

Keywords:
AeolianDuneMarsMegaripplesMigrationRipples

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Area of Science:

  • Planetary Science
  • Aeolian Geomorphology
  • Mars Surface Processes

Background:

  • Aeolian megaripples, with spacings of 5-50m, are common Martian surface features.
  • Previously, megaripples, especially bright Transverse Aeolian Ridges (TARs), were considered relict features due to a lack of observed movement.
  • High-resolution orbital imagery has historically failed to detect megaripple migration.

Purpose of the Study:

  • To investigate the activity and migration of Martian megaripples, particularly bright-toned ones (TARs).
  • To determine if megaripples and small TARs are active geological features in the present Martian climate.
  • To analyze sand flux associated with active megaripples and compare it to dune activity.

Main Methods:

  • Targeted high-resolution orbital imaging of two equatorial Martian regions: Syrtis Major and Mawrth Vallis.
  • Analysis of megaripple spacing, ranging from 1 to 35m (average 5m).
  • Quantification of sand flux for observed migrating megaripples and comparison with surrounding dunes.

Main Results:

  • Evidence of migration was found for bright-toned megaripples in Syrtis Major and Mawrth Vallis.
  • Active megaripples exhibit sand fluxes two orders of magnitude lower than surrounding dunes.
  • Martian megaripples can migrate obliquely and longitudinally, differing from terrestrial counterparts.

Conclusions:

  • Megaripples and small Transverse Aeolian Ridges (TARs) are active features on present-day Mars.
  • Their activity suggests a past climate with a denser atmosphere is not required for their formation or migration.
  • Active megaripples, alongside high-sand flux dunes, serve as key indicators of strong surface winds on Mars.