Related Experiment Video
Updated: Aug 5, 2026

09:49
Prospecting Microbial Strains for Bioremediation and Probiotics Development for Metaorganism Research and Preservation
Published on: October 31, 2019
Ultrastructural changes in an obligately barophilic marine bacterium after decompression
1Scripps Institution of Oceanography (A-002), University of California, San Diego, La Jolla, California 92093-0202.
Applied and Environmental Microbiology
|May 1, 1991
Summary
Deep-sea bacteria (MT-41) undergo significant morphological changes and cell death when decompressed to atmospheric pressure. Proper sample fixation is crucial for accurate hadal zone research.
Area of Science:
- Microbiology
- Oceanography
- Cell Biology
Background:
- The bacterial isolate MT-41 was obtained from a depth of 10,476 meters.
- MT-41 is an obligately barophilic bacterium, meaning it requires high pressure to survive.
Purpose of the Study:
- To investigate the morphological alterations of MT-41 following decompression from high hydrostatic pressure to atmospheric pressure.
- To observe the effects of prolonged incubation at atmospheric pressure on the cell structure and viability of MT-41.
Main Methods:
- Cultures of MT-41 were grown at 103.5 MPa and 2°C.
- Cultures were decompressed to 0.101 MPa (atmospheric pressure).
- Morphological and ultrastructural changes were assessed via microscopy at various time points post-decompression, with viability assessed by colony-forming units (CFU).
Main Results:
- Decompression did not cause immediate morphological changes, but prolonged exposure to atmospheric pressure led to significant ultrastructural degradation.
- Observed changes included intracellular vesicles, membrane fragments, plasmolysis, cell lysis, extracellular vesicle formation, and ghost cells.
- Bacterial viability (CFU) decreased over time at atmospheric pressure, and nucleoid fibrils were poorly stained in surviving cells.
Conclusions:
- Hadal deep-sea bacteria are highly sensitive to pressure changes.
- Immediate in situ or surface fixation of deep-sea samples is essential to prevent structural degradation and ensure accurate ecological assessments.
More Related Videos
Related Concept Videos
Bacterial Phylum Cyanobacteria
Cyanobacteria are a diverse group of oxygenic, phototrophic bacteria that played a pivotal role in converting Earth’s atmosphere from anoxic to oxygen-rich billions of years ago. They exhibit remarkable morphological diversity, ranging from unicellular forms to filamentous types, with cell sizes varying between 0.5 μm and 100 μm. Cyanobacteria are classified into five groups: Chroococcales (unicellular, dividing by binary fission), Pleurocapsales (unicellular, dividing by multiple fission),...
Anoxygenic Phototrophic Bacteria
Anoxygenic phototrophic bacteria are a diverse group of microorganisms that perform photosynthesis without producing oxygen. They primarily include purple sulfur bacteria, purple nonsulfur bacteria, green sulfur bacteria, and green nonsulfur bacteria. These bacteria are classified into the Gammaproteobacteria, Alphaproteobacteria, Betaproteobacteria, Chlorobi, and Chloroflexi lineages, each with distinct physiological and ecological adaptations.Purple sulfur bacteria belong to the...
Diversity of Archaea III
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 environments.Morphological...
Microbial Mats
Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...
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 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...

