Borzan Vladimir, Tomašević Boris, Kurbel Sven
Osijek University Hospital, Dept. of Internal Medicine, Osijek, Croatia.
Zagreb University Hospital, Dept. of Anesthesiology, Zagreb, Croatia.
J Theor Biol. 2014 Dec 21;363:164-8. doi: 10.1016/j.jtbi.2014.08.015. Epub 2014 Aug 21.
This paper puts forward a new hypothesis to interpret the high carrier frequency of CFTR mutations in individuals of European descent. The proposed heterozygote advantage factor is related to the specific climate conditions in Europe during the last 50 ky that might have heavily compromised the respiratory function of our ancestors in Eurasia. A large part of the last 50 ky was cold, and the coldest period was the Last Glacial Maximum (LGM) (26.5 to 19 kya). The global climate was dry with a dust-laden atmosphere (20 to 25 times more dust than the present level). High levels of atmospheric dust started more than 40 kya and ended less than 10 kya. Secretion of airway fluid is usually related to the submucosal tissue hydration, while salt reabsorption relies on activation of CFTRs that allow ENaCs to absorb salt and water. The water loss by evaporation depends on the air humidity and flow rate. Salt accumulation in the mucus is normally prevented by reabsorption of Na(+) and Cl(-) by epithelial cells if the presence of functional CFTRs is normal. If one gene for CFTR is mutated, the number of functional CFTRs is reduced and this limits the capacity of salt reabsorption by epithelial cells. This means that evaporation makes the airway fluid more hypertonic, and osmotic forces bring more water from the interstitial space, thus leading to a new balance in mucosal fluid traffic. Increased osmolarity and volume of airway fluid can be more moveable in cases when evaporation and dust exposure is increased. If both CFTR genes are mutated, low number of functional CFTRs diminishes salt resorption of epithelial cells. Salt accumulated in the mucous fluid within respiratory ducts, as previously described. The hypertonic ductal content forces more water and some electrolytes to enter the airway fluid from the interstitial fluid, and evaporation leads to further concentration of thick immobile mucus. The proposed interpretation is that CFTR mutations have spread among our ancestors that roamed the central Eurasia after the LGM. The heterozygote individuals might have benefitted from the limited water resorption in their respiratory mucosa that allowed improved airway cleansing.
本文提出了一个新的假说,以解释欧洲血统个体中CFTR突变的高携带频率。所提出的杂合子优势因素与过去5万年欧洲的特定气候条件有关,这些条件可能严重损害了我们欧亚大陆祖先的呼吸功能。过去5万年的大部分时间是寒冷的,最冷的时期是末次盛冰期(LGM)(26.5至19千年前)。全球气候干燥,大气中充满尘埃(比目前水平多20至25倍)。高浓度的大气尘埃始于4万多年前,结束于不到1万年前。气道液体的分泌通常与黏膜下组织的水合作用有关,而盐的重吸收则依赖于CFTR的激活,CFTR允许ENaC吸收盐和水。蒸发导致的水分流失取决于空气湿度和流速。如果功能性CFTR的存在正常,上皮细胞对Na(+)和Cl(-)的重吸收通常可以防止黏液中盐分的积累。如果一个CFTR基因发生突变,功能性CFTR的数量就会减少,这就限制了上皮细胞重吸收盐分的能力。这意味着蒸发会使气道液体变得更加高渗,渗透压会从间质空间带来更多的水,从而导致黏膜液体运输达到新的平衡。在蒸发增加和接触尘埃的情况下,气道液体渗透压和体积的增加会使其更易于流动。如果两个CFTR基因都发生突变,功能性CFTR数量的减少会削弱上皮细胞的盐重吸收能力。如前所述,呼吸道导管内的黏液中会积累盐分。高渗的导管内容物迫使更多的水和一些电解质从间质液进入气道液体,蒸发会导致浓稠的不流动黏液进一步浓缩。所提出的解释是,CFTR突变在末次盛冰期之后在我们游荡于欧亚大陆中部的祖先中传播开来。杂合子个体可能从其呼吸道黏膜中有限的水分重吸收中受益,这使得气道清洁得到改善。