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Late Pleistocene-Holocene deltas in southern Buenos Aires Province, Argentina

机译:已故的普齐罗涅 - 全新世德尔塔斯在南布宜诺斯艾利斯省,阿根廷省

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Along the Argentina coast there are only two present day deltas, the Parana and Colorado deltas, both located in Buenos Aires Province. However, the Colorado Delta is only a minor remnant of a much larger delta system that was active from approximately 10 000 calibrated years BP, when mean sea level (msl) was about -30 m. Based on bathymetric and topographic maps, regional geology and bibliography, the evolution of the delta system is proposed. During the Last Glacial Maximum (LGM), 24 000 calibrated years BP, msl was -130 m, located at the present shelf break. During this period the fluvial drainage was minimum. As climate conditions changed, it can be deduced from well preserved terraces that the msl increased in pulses. The uppermost terrace, located at -25/-30 m corresponds to the deltaic front of the Colorado and Negro rivers. At this time, the fluvial discharge was large and a series of rivers (most of them no longer existing today) provided sediments to the deltas. The Colorado River and a set of unnamed rivers were active to the northern and central portion of this 430 km delta front, whereas the Negro River provided materials to the lower central and southern portions. We estimate that the major sediment and water inputs occurred at about 9000 calibrated years BP, when msl was -18 m. Delta evolution was significantly modified when msl was up to 6 m above the present, 6000 calibrated years BP. At this time, both the Colorado and Negro rivers migrated southward. Msl decreased at about 4 mm/year until it reached the lowest level, about -2 m during the Little Ice Age. Today, the only active delta is the one maintained by a diminished Colorado River in the central part of the area. The northern and southern portions are now extensive intertidal areas with remnant islands and large tidal channels corresponding, respectively, to Bahia Blanca Estuary and Anegada Bay. The Negro River has an estuary at its mouth but no delta is active today.
机译:沿着阿根廷海岸,只有两天的Deltas,Parana和Colorado Deltas,都位于布宜诺斯艾利斯省。然而,Colorado Delta只是一个很多较大的Delta系统的次要残余,当平均海平面(MSL)约为-30米时,从大约10 000次校准年龄为大约10 000次校准的年龄。基于碱基和地形图,区域地质学和参考书目,提出了DELTA系统的演变。在上次冰川最大(LGM)期间,24 000次校准年BP,MSL为-130米,位于当前货架突破。在此期间,河流排水最小。随着气候条件的变化,它可以从保存的露台推导出MSL在脉冲中增加。最重要的露台,位于-25 / -30 m,对应于科罗拉多州和黑人河的红角洲前面。此时,河流放电很大,一系列河流(今天的大多数人不再存在)为谵妄提供了沉积物。科罗拉多河和一套未命名的河流在这430公里的三角洲前面的北部和中央部分处于活跃状态,而黑人河则为下部中央和南部的部分提供材料。当MSL为-18米时,我们估计主要沉积物和水投入发生在约9000次校准年龄BP。当MSL高达6米以上时,6000次校准多年BP时,Delta Evolutize显着修改。此时,科罗拉多州和黑人河都遍布向南迁移。 MSL在大约4毫米/年下降,直到它达到最低水平,在小冰河时代约为-2米。今天,唯一的活跃三角洲是由该地区的中央部分的Colorado河维护的唯一。北部和南部的部分现在是广泛的跨境地区,分别具有残余岛屿和大型潮汐渠道,分别对应于巴伊亚布兰卡河口和安格达湾。黑人河嘴里有一个河口,但今天没有三角洲活跃。

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