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仲德林等通过卫片解释研究了古长江口的演化问题,提出了从东台到江都在全新世早期的古长江口演化也存在“雁”形演化这一新看法。本刊认为,这种看法是对玉木冰期低海面时长江三角洲可能位于东海水深150米以下这一概念的挑战,并有可能建立起自全新世以来长江三角洲演化的基本模式。这是一个值得注意的科研动向。我们热切希望有关这方面进一步的研究成果,更多地出现在本刊上。
Zhong Delin et al. Studied the evolution of the ancient Yangtze Estuary through the interpretation of the satellites and proposed that the evolution of the Yangtze River Mouth during the early Holocene from Dongtai to Jiangdu also had the new view of “geese” evolution. Our view is that this view is a challenge to the notion that the Yangtze River Delta may be located 150 meters below the sea level in the East China Sea at the time of the low sea level of the Tamagushi Ice Age and is likely to establish the basic model for the evolution of the Yangtze River delta since the Holocene. This is a noteworthy research trend. We sincerely hope that further research on this topic will appear more in this magazine.