Laurent Pierre, Chevalier Claudine, Wood Chris M
Department of Biology, McMaster University, 1280 Main Street West, L8S 4K1, Hamilton, ON, Canada.
Cell Tissue Res. 2006 Sep;325(3):481-92. doi: 10.1007/s00441-006-0187-3. Epub 2006 Apr 26.
Fundulus heteroclitus (killifish) is a model organism for ionoregulatory studies, particularly because of its opercular epithelium, although the gills are the major sites of ion exchange. Whereas Na+ and Cl- are excreted through the gills in seawater (SW), the killifish is unusual in taking up only Na+ and not Cl- at the gills in freshwater (FW). We describe morphological changes in the branchial epithelium following transfer from an acclimation medium of 10% SW to 100% SW or FW. In 10% SW, mitochondria-rich cells resemble typical seawater chloride cells (SWCCs) with accessory cells. After transfer to 100% SW, no change occurs in pavement cell (PVC) morphology or mitotic rate (measured by bromo-deoxyuridine technique), although the density of SWCC apertures increases several fold because of the uncovering of buried SWCCs by PVCs, in accord with increased rates of Na+ and Cl- efflux. After transfer to FW, PVC morphology remains unchanged, but SWCCs and accessory cells are quickly covered by PVCs, with many undergoing apoptosis or necrosis. The mitotic rate doubles by 10-14 h but typical freshwater chloride cells (FWCCs) do not appear. Instead, a wedge-shaped cell type that is moderately rich in apically oriented mitochondria, with a large ovoid nucleus, thin cytoplasmic layer, paucity of vesicular-tubular network, and variably villous surface rapidly (by 3 h) and progressively appears in the filament epithelium, by both uncovering and mitosis. This cell type is similar to that recently identified as the site of Na+ uptake in the FW trout gill. We propose the new term "cuboidal cell" for this cell, based on its morphology, to avoid confusion with traditional terminology (of PVC). We hypothesize that the cuboidal cells are the sites of active Na+ uptake in FW F. heteroclitus and suggest that the lack of Cl- uptake is attributable to the absence of typical FWCCs previously described in teleosts.
底鳉是离子调节研究的模式生物,特别是因其鳃盖上皮,尽管鳃是离子交换的主要部位。在海水中,Na⁺和Cl⁻通过鳃排出,但底鳉在淡水中仅摄取Na⁺而不摄取Cl⁻,这一点很不寻常。我们描述了从10%海水的驯化培养基转移到100%海水或淡水后鳃上皮的形态变化。在10%海水中,富含线粒体的细胞类似于带有辅助细胞的典型海水氯化物细胞(SWCCs)。转移到100%海水后,扁平细胞(PVC)的形态或有丝分裂率(通过溴脱氧尿苷技术测量)没有变化,尽管由于PVCs揭开了埋藏的SWCCs,SWCC孔的密度增加了几倍,这与Na⁺和Cl⁻流出率的增加一致。转移到淡水后,PVC形态保持不变,但SWCCs和辅助细胞很快被PVCs覆盖,许多细胞发生凋亡或坏死。有丝分裂率在10 - 14小时内翻倍,但典型的淡水氯化物细胞(FWCCs)没有出现。相反,一种楔形细胞类型迅速(3小时内)并逐渐出现在鳃丝上皮中,这种细胞类型顶端朝向的线粒体适度丰富,有一个大的卵圆形细胞核,细胞质层薄,泡管状网络稀少,表面有可变的绒毛,通过揭开和有丝分裂形成。这种细胞类型类似于最近在淡水虹鳟鱼鳃中被确定为Na⁺摄取部位的细胞类型。基于其形态,我们为这种细胞提出了新术语“立方形细胞”,以避免与传统术语(PVC)混淆。我们假设立方形细胞是淡水底鳉中活跃摄取Na⁺的部位,并认为缺乏Cl⁻摄取是由于硬骨鱼中先前描述的典型FWCCs不存在。