Centre for Trophoblast Research, University of Cambridge, Cambridge, UK.
Department of Physiology, Development and Neuroscience, University of Cambridge, Cambridge, UK.
Reproduction. 2021 Jan;161(1):F53-F65. doi: 10.1530/REP-20-0153.
Development of the human placenta takes place in contrasting oxygen concentrations at different stages of gestation, from ~20 mmHg during the first trimester rising to ~60 mmHg at the start of the second trimester before gradually declining to ~40 mmHg at term. In view of these changes, the early placenta has been described as 'hypoxic'. However, placental metabolism is heavily glycolytic, supported by the rich supply of glucose from the endometrial glands, and there is no evidence of energy compromise. On the contrary, the trophoblast is highly proliferative, with the physiological low-oxygen environment promoting maintenance of stemness in progenitor populations. These conditions favour the formation of the cytotrophoblastic shell that encapsulates the conceptus and interfaces with the endometrium. Extravillous trophoblast cells on the outer surface of the shell undergo an epithelial-mesenchymal transition and acquire invasive potential. Experimental evidence suggests that these changes may be mediated by the higher oxygen concentration present within the placental bed. Interpreting in vitro data is often difficult, however, due to the use of non-physiological oxygen concentrations and trophoblast-like cell lines or explant models. Trophoblast is more vulnerable to hyperoxia or fluctuating levels of oxygen than to hypoxia, and some degree of placental oxidative stress likely occurs in all pregnancies towards term. In complications of pregnancy, such as early-onset pre-eclampsia, malperfusion generates high levels of oxidative stress, causing release of factors that precipitate the maternal syndrome. Further experiments are required using genuine trophoblast progenitor cells and physiological concentrations to fully elucidate the pathways by which oxygen regulates placental development.
人类胎盘的发育发生在妊娠不同阶段的对比氧浓度中,从孕早期的20mmHg 上升到孕中期开始时的60mmHg,然后逐渐下降到足月时的~40mmHg。鉴于这些变化,早期胎盘被描述为“缺氧”。然而,胎盘代谢主要是糖酵解,子宫内膜腺体提供丰富的葡萄糖供应,没有能量不足的证据。相反,滋养层具有高度增殖性,生理低氧环境促进祖细胞群体的干性维持。这些条件有利于形成包裹胚胎和与子宫内膜接口的细胞滋养层壳。壳外的绒毛外滋养层细胞经历上皮-间充质转化并获得侵袭潜力。实验证据表明,这些变化可能是由胎盘床内存在的较高氧浓度介导的。然而,由于使用非生理氧浓度以及滋养层样细胞系或外植体模型,解释体外数据通常很困难。与缺氧相比,滋养层对高氧或氧波动更敏感,并且在所有妊娠接近足月时,胎盘可能会发生一定程度的氧化应激。在妊娠并发症中,如早发型子痫前期,灌注不良会产生高水平的氧化应激,导致释放引发母体综合征的因子。需要进一步使用真正的滋养层祖细胞和生理浓度的实验来充分阐明氧调节胎盘发育的途径。