Carbonates
multipolar
bony fishes
bony fishes
bony fishes
Silicate minerals are the most abundant class of minerals on Earth. They are composed of silicon and oxygen atoms, and form the majority of the Earth's crust. Examples include quartz, feldspar, and mica.
Silicates are more common in Earth's crust and mantle compared to nonsilicates. They make up about 90% of the Earth's crust and include a wide variety of minerals such as quartz, feldspar, and mica. Nonsilicate minerals, while important, are less abundant and include categories like carbonates, oxides, and sulfates. Overall, the predominance of silicate minerals is a key characteristic of Earth's geology.
The most abundant and diverse members of the class Osteichthyes, commonly known as bony fish, are the teleosts. Teleosts make up the majority of fish species, with over 30,000 identified, including familiar groups such as salmon, tuna, and goldfish. Their evolutionary adaptations, such as specialized feeding mechanisms and varied reproductive strategies, contribute to their vast diversity and ecological success in aquatic environments.
The most abundant class of neuron in the central nervous system is the interneuron. Interneurons are responsible for forming connections between sensory and motor neurons, allowing for communication within the central nervous system to process information and generate appropriate responses.
The most abundant and diverse vertebrates in the class Osteichthyes are the ray-finned fish (Actinopterygii). They are found in a wide range of aquatic environments and exhibit a high degree of diversity in terms of size, shape, and behavior. Examples include tuna, trout, and goldfish.
most abundant shark
The antibody class that is most abundant in plasma and is crucial for fixing complement is Immunoglobulin G (IgG). It is also the only antibody class that can cross the placenta, providing passive immunity to the newborn. This transfer of IgG helps protect the infant from infections during the early months of life.
Igneous. Basalt is the most abundant in oceanic crust and granite is the most abundant in continental crust.