Biologists use microscopes and tools of biochemistry to study cells.
Eukaryotic cells have internal membranes that compartmentalize their functions.
Mitochondria and chloroplasts change energy from one form to another, and have an interesting prokaryotic evolutionary origin.
Some groups survived and adapted using cellular respiration to harvest energy.
Most atmospheric oxygen (O2) is of biological origin.
O2 produced by oxygenic photosynthesis reacted with dissolved iron and precipitated out to form banded iron formations.
By about 2.7 billion years ago, O2 began accumulating in the atmosphere and rusting iron-rich terrestrial rocks, a process known as the "oxygen revolution".
The initial rise in O2 was likely caused by ancient cyanobacteria.
The "oxygen revolution" caused extinction of many prokaryotic groups.
Later increases in atmospheric O2 might have been caused by the evolution of eukaryotic cells containing chloroplasts.
In a light microscope (LM), visible light is passed through a specimen and then through glass lenses, which refract (bend) the light, so that the image is magnified.
The size range of cells can be explored using microscopy.
Three important parameters of microscopy are magnification, resolution, and contrast.
Magnification is the ratio of an object’s image size to its real size, making something appear bigger.
Resolution is the measure of clarity of the image, determining if two separate points on the image can be distinguished.
Contrast is the visibility of differences in parts of the sample, determining if a feature can be distinguished from the background.
The endosymbiotic theory suggests that an early ancestor of eukaryotes engulfed an aerobic (oxygen-using) nonphotosynthetic prokaryote.
Peroxisomes are oxidative organelles, using oxygen for some molecular breakdown, forming peroxides but also converting those peroxides into water, protecting other cellular components.
Prokaryotes were Earth’s sole inhabitants from 3.5 to about 2.1 billion years ago.
A second endosymbiotic event involved a photosynthetic prokaryote being engulfed by a eukaryote containing mitochondria.
The Phanerozoic is divided into three eras: the Paleozoic, Mesozoic, and Cenozoic.
Chloroplasts, found in plants and algae, are the site of photosynthesis, a metabolic process that uses the energy from sunlight to fix carbon (from CO2) and uses it to generate energy-rich organic molecules such as glucose.
The Phanerozoic includes the last half billion years, and encompasses multicellular eukaryotic life.
The engulfed prokaryote was maintained within the host cell and became an endosymbiont, eventually evolving into a mitochondrion.
Mitochondria are the site of cellular respiration, a metabolic process that uses oxygen to generate ATP.
This endosymbiont evolved into a chloroplast.
Energy-transducing mitochondria and chloroplasts are not part of the endomembrane system, and are derived from prokaryotes.
Stromatolites date back 3.5 billion years ago.
The oldest known fossils are stromatolites, rocks formed by the accumulation of sedimentary layers on bacterial mats.
Mitochondria and chloroplasts change energy from one form to another.
Light Microscopy (LM) magnifies effectively to about 1,000 times the size of the actual specimen.
Various techniques enhance contrast and enable cell components to be stained or labelled in Light Microscopy.
Most subcellular structures, like organelles, are too small to be resolved by standard Light Microscopy.
In Brightfield (Unstained) Light Microscopy, light directly passes through the specimen, resulting in little contrast, unless the cells are pigmented or stained.
In Brightfield (Stained) Light Microscopy, staining enhances contrast and cells are fixed and stained (and therefore killed) in most staining procedures.
Recent advances in light microscopy include confocal microscopy and deconvolution microscopy, which provide sharper images of 3-D tissues and cells.
Both types of electron microscopes focus a beam of electrons using electromagnets rather than lenses.
Confocal microscopy uses a laser to produce sharper images and allows 3-D image reconstruction by 'optical sectioning' and reconstructing images from different planes.
The surface of SEM specimens is usually covered in a thin film of gold, and the electron beam excites the surface electrons.