北黄海盆地中侏罗世-早白垩世构造体制转换期的古气候演化及元素地球化学响应

中侏罗世-早白垩世华北地台东部的北黄海盆地受古亚洲构造体制向滨太平洋构造体制转换的影响，其构造演化经历了伸展-反转挤压-伸展的转变.构造体制的差异不但表现在大地构造性质及其产生的地质效应上，也表现在盆地沉积特征、古生物及古气候等方面.本文以北黄海盆地东部坳陷X1井中侏罗统至下白垩统为研究对象，利用泥岩元素地球化学特征对古气候的指示，结合盆地沉积特征及古生物资料，对古气候演化展开研究.研究显示，中侏罗世-早白垩世X1井泥岩样品的Sr/Cu比值（2.12~34.10）、Sr/Ba比值（0.16~1.60）、Rb/Sr比值（0.13~1.23）、Fe₂O₃/FeO比值（0.22~11.10）、V/Cr比值（0.91~1.78）、V/Sc比值（4.89~8.33）、Ni/Co比值（1.14~3.85）、δU比值（0.50~0.84）和U/Th比值（0.11~0.24）的纵向变化反映古气候经历了温湿→整体湿润、短暂干热→干热的演化.沉积物经历了暗色细粒沉积物为主→灰色、灰色夹灰绿色、灰色与红褐色互层细粒沉积物为主→灰色粗粒沉积物和红褐色、灰黄色细粒沉积物为主的变化.古生物经历了喜湿植物丰富→喜热植物出现→喜热植物丰富的过程.结果表明，受古亚洲构造体制和滨太平洋构造体制的影响，华北地台向北漂移，北黄海盆地古气候经历了由中侏罗世-晚侏罗世早期以温湿气候为主，至晚侏罗世晚期-早白垩世早期整体相对湿润，出现短暂干热气候，到早白垩世中期-早白垩世晚期为干热气候的演化.北黄海盆地中侏罗世-早白垩世古气候由温湿向干热的转变正是对华北地台东部晚中生代两大构造体制转换的响应. 

Paleoclimate Evolution and Elemental Geochemical Response during Middle Jurassic-Early Cretaceous in Tectonic Regime Transition Period in the North Yellow Sea Basin

The North Yellow Sea basin in the eastern part of the North China platform from the Middle Jurassic to the Early Cretaceous was influenced by the transformation from Paleo-Asian tectonic system to Marginal Pacific tectonic system, and its tectonic evolution experienced transformations of extension-compression-extension. The differences of tectonic systems are shown not only in the geotectonic properties and their geological effects, but also in the sedimentary characteristics of the basin, paleontology and paleoclimate. In this paper, the Middle Jurassic to Lower Cretaceous of the well X1 in the eastern depression of the North Yellow Sea basin is taken as the research object, and the paleoclimate evolution is studied by using the indication of mudstone element geochemical characteristics to paleoclimate, combined with basin sedimentary characteristics and paleobiological data. Research results show that, the longitudinal changes of Sr/Cu(2.12-34.10), Sr/Ba(0.16-1.60), Rb/Sr(0.13-1.23), Fe₂O₃/FeO(0.22-11.10), V/Cr(0.91-1.78), V/Sc(4.89-8.33), Ni/Co(1.14-3.85), δU(0.50-0.84), U/Th(0.11-0.24) from the Middle Jurassic to the Early Cretaceous reflect that the paleoclimate evolution experienced variations from warm and humid to whole humid, short dry and hot to dry and hot. The sediments experienced the main changes form dark fine-grained sediments to gray, gray interbedded with gray-green, gray and reddish brown interbedded fine sediments to gray coarse-grained sediments and reddish-brown and grayish-yellow fine-grained sediments. Paleontology experienced the process of abundance of hygrophilous plants-appearance of heat-loving plants-abundance of heat-loving plants. The results show that the North China platform drifted northward due to the influence of Paleo-Asian tectonic system and Marginal Pacific tectonic system. At the same time, the paleoclimate evolution of the North Yellow Sea basin underwent a dramatic change from the Middle Jurassic to the late Late Cretaceous; during the Middle Jurassic to the early Late Jurassic, it was dominated by warm and humid climate; from the late Late Jurassic to the early Early Cretaceous the whole climate was relatively wet, with a short dry and hot climate; from the middle Early Cretaceous to the late Early Cretaceous it was dry and hot climate. The paleoclimate in the North Yellow Sea basin has experienced the evolution from a warm and humid climate to dry and hot climate during the Middle Jurassic-the Early Cretaceous, which is a response to the transformation of two major Mesozoic tectonic regimes in the east of North China platform.