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Related Concept Videos

Marine Microbial Ecology01:30

Marine Microbial Ecology

Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Deep Sea Microbial Ecology01:18

Deep Sea Microbial Ecology

The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...
Microenvironments01:22

Microenvironments

Microorganisms inhabit highly localized spaces known as microenvironments, which are defined by distinct physical and chemical characteristics. These include oxygen concentration, pH, temperature, light availability, and nutrient levels. The conditions within a microenvironment can differ markedly from those in the surrounding area and significantly influence microbial growth, metabolism, and community structure.Microenvironments often display sharp physicochemical gradients over small spatial...
The Colloidal State01:29

The Colloidal State

The formation of a colloidal system is exemplified by an aqueous solution containing Cl− ions is introduced to another containing Ag+ ions, resulting in the precipitation of solid AgCl as extremely tiny crystals. Instead of settling out as a filterable precipitate, these crystals remain suspended in the liquid, showcasing a colloidal system.A colloidal system involves colloidal particles within the approximate range of 1 to 1000 nm in at least one dimension, dispersed in a medium called the...
Microbes and Other Elemental Cycles01:24

Microbes and Other Elemental Cycles

Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
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Colloids and Suspensions

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Related Experiment Video

Updated: Jul 12, 2026

An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles
09:01

An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles

Published on: April 19, 2018

The oceanic microcosm of particles.

D Lal

    Science (New York, N.Y.)
    |December 9, 1977
    PubMed
    Summary

    Ocean particles influence chemical processes by scavenging trace elements and releasing others like carbon and silicon. Understanding these particle dynamics is crucial for ocean chemistry research.

    Area of Science:

    • Marine chemistry
    • Geochemistry
    • Oceanography

    Background:

    • Suspended particulate matter plays a key role in ocean biogeochemical cycles.
    • Previous studies have highlighted the importance of particle-seawater interactions.

    Purpose of the Study:

    • To investigate the chemical processes associated with suspended particulate matter in the Atlantic and Pacific oceans.
    • To understand the role of particles in controlling trace element concentrations and introducing other elements.

    Main Methods:

    • Analysis of suspended particulate matter (>1 micrometer) collected during GEOSECS expeditions.
    • Filtration of large volumes of surface and deep ocean water.
    • Measurement of trace element and radionuclide concentrations on particulate matter.

    More Related Videos

    Chemotactic Response of Marine Micro-Organisms to Micro-Scale Nutrient Layers
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    Chemotactic Response of Marine Micro-Organisms to Micro-Scale Nutrient Layers

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    Protocol for Microplastics Sampling on the Sea Surface and Sample Analysis
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    Protocol for Microplastics Sampling on the Sea Surface and Sample Analysis

    Published on: December 16, 2016

    Related Experiment Videos

    Last Updated: Jul 12, 2026

    An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles
    09:01

    An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles

    Published on: April 19, 2018

    Chemotactic Response of Marine Micro-Organisms to Micro-Scale Nutrient Layers
    22:38

    Chemotactic Response of Marine Micro-Organisms to Micro-Scale Nutrient Layers

    Published on: May 28, 2007

    Protocol for Microplastics Sampling on the Sea Surface and Sample Analysis
    10:16

    Protocol for Microplastics Sampling on the Sea Surface and Sample Analysis

    Published on: December 16, 2016

    Main Results:

    • Particles act as a scavenger, removing trace elements (Th, Pu, Fe, Pb, Cu) from the ocean column.
    • Particles serve as a source for elements like carbon and silicon, released upon dissolution at depth.
    • Particulate concentrations and fluxes are both critical for understanding ocean chemical processes.

    Conclusions:

    • Particulate matter significantly influences ocean chemical composition and element cycling.
    • Both scavenging of elements by particles and release from dissolving particles are important processes.
    • Integrated studies of particulate concentration and flux are necessary for a comprehensive understanding of marine chemical processes.