MACRO - The Centre for Macroalgal Resources and Biotechnology, College of Marine and Environmental Sciences, James Cook University, Townsville 4811, Australia; Environmental Research Institute, School of Science, University of Waikato, Tauranga 3110, New Zealand.
The Ferrier Research Institute, Victoria University of Wellington, 69 Gracefield Road, Lower Hutt 5010, New Zealand.
Int J Biol Macromol. 2022 Jan 1;194:571-579. doi: 10.1016/j.ijbiomac.2021.11.100. Epub 2021 Nov 20.
Ulvans from Ulva ohnoi, Ulva tepida and Ulva prolifera were extracted under mild acidic conditions, isolated and their composition and structure determined. The ulvans contained mostly rhamnose (31.6-46.7 mol%) and glucuronic acid (26.6-37.5 mol%), with smaller amounts of xylose (3.4-10.4 mol%) and iduronic acid (3.1-7.6 mol%). In addition, the ulvan samples also contained galactose (4.4-26.0 mol%). Glycosyl linkage analysis showed that ulvan from U. ohnoi contained mostly →4)-GlcpA-(1→ and →3,4)-Rhap-(1→. Preparation of partially methylated alditol acetate standards of idose showed that U. ohnoi contained →4)-IdopA-(1→. In addition to these residues, glycosyl linkage analysis of U. tepida and U. prolifera showed the presence of →2,3,4)-Rhap-(1→, →4)-Xylp-(1→, →2,4)-GlcpA-(1→ and →3,4)-GlcpA-(1→. These two species also contained galactose linkages. These data, together with nuclear magnetic resonance (NMR) spectroscopy indicated that U. ohnoi comprised mostly of type A ulvanobiuronic acid repeats [→4)-β-D-GlcpA-(1→4)-α-L-Rhap3S-(1→], together with smaller amounts of type B ulvanobiuronic acid repeats [→4)-α-L-IdopA-(1→4)-α-L-Rhap3S-(1→] and ulvanobiose (U [→4)-β-D-Xylp-(1→4)-α-L-Rhap3S-(1→]). NMR spectra of U. tepida and U. prolifera showed resonances not detected in U. ohnoi, highlighting the complexity of the ulvans from these species. Regardless of the structural diversity of the ulvan samples there was very little antioxidant or inhibitory activity detected on enzymatic processes investigated.
从孔石莼、条浒苔和石莼中提取了温和酸性条件下的岩藻聚糖,并对其进行了分离和组成及结构的测定。岩藻聚糖主要含有鼠李糖(31.6-46.7mol%)和葡萄糖醛酸(26.6-37.5mol%),少量木糖(3.4-10.4mol%)和艾杜糖醛酸(3.1-7.6mol%)。此外,岩藻聚糖样品还含有半乳糖(4.4-26.0mol%)。糖苷键分析表明,孔石莼岩藻聚糖主要含有→4)-GlcpA-(1→和→3,4)-Rhap-(1→。部分甲基化糖醇乙酸酯标准物的制备表明,孔石莼含有→4)-IdopA-(1→。除了这些残基,浒苔和石莼的糖苷键分析表明存在→2,3,4)-Rhap-(1→,→4)-Xylp-(1→,→2,4)-GlcpA-(1→和→3,4)-GlcpA-(1→。这两个物种还含有半乳糖键。这些数据与核磁共振(NMR)光谱一起表明,孔石莼主要由 A 型岩藻聚糖重复单元组成[→4)-β-D-GlcpA-(1→4)-α-L-Rhap3S-(1→],同时还含有少量 B 型岩藻聚糖重复单元[→4)-α-L-IdopA-(1→4)-α-L-Rhap3S-(1→]和岩藻聚糖二糖(U [→4)-β-D-Xylp-(1→4)-α-L-Rhap3S-(1→]。浒苔和石莼的 NMR 谱显示了孔石莼中未检测到的共振峰,突出了这些物种岩藻聚糖的复杂性。无论岩藻聚糖样品的结构多样性如何,在所研究的酶促过程中检测到的抗氧化或抑制活性都非常少。