The phrase "aging evolution" is not commonly used in written English and may be unclear in meaning.
It could be used in contexts discussing the process of aging in relation to evolutionary biology or the changes in species over time as they age.
Example: "The study of aging evolution reveals how certain traits are preserved or discarded as species adapt to their environments over generations."
Alternatives: "evolution of aging" or "evolutionary aging process".
Moreover, since many stress response mechanisms are broadly conserved, data obtained at the microbial scale may facilitate the comprehension of complex phenomena, such as aging, evolution of neurological diseases and cancer.
Based on this idea we propose experimental schemes for aging, evolution and biomedical research.
Based on this idea we will also allude to experimental schemes for aging, evolution and biomedical research.
The biological aging process was studied in China by Bai and co-workers and among 208 physical, morphological, physiological and biochemical variables, only eight were chosen as candidate biomarkers of aging, which included echocardiographic parameters, intima-media thickness (IMT) and fibrinogen, demonstrating its importance on aging evolution [ 11].
Because they are part of the constant bombardment from free space to which all matter is constantly exposed, however, they may have considerable effects, such as contributing to the processes of aging and evolution.
The monumental work of Medawar stems from his long and deep interest in the nature of living organisms' changes over time, such as growth, aging, and evolution.
Previously published experiments on aging and evolution may also benefit from reanalysis in the light of life-history senemorphism.
During atmospheric aging the evolution of size and composition of primary particles, i.e. particles that enter the atmosphere in the condensed phase, is influenced by condensation and evaporation of vapors.
This paper focuses on the early age evolution of consistency and rheological properties of fresh bitumen emulsion-cement (BEC) pastes.
Thus, a reconstruction of the landscape history of the Wae Racang valley using speleothems, geological structure, tectonic uplift, karst, cave, and terrace development, provides the necessary evidence to determine the formation, age, evolution, and influences on the site.
The late-Holocene, especially post-Little Ice Age, evolution of Nystølen alluvial fan, Langedalen, Jostedalsbreen region, southern Norway, is investigated using a combination of evidence from surface morphology, recent aerial photography, lichenometric dating, hydrological reconstruction, stratigraphy, and sedimentology.
