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2022 Wetlands Guide for Web - single pages

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44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 44 GUIDE TO NEBRASKA'S WETLANDS Riverine Wetlands W etlands are closely associated with the riparian zones (the interface between land and a river or stream) and associated fl oodplains (areas formed mainly of river sediments and subject to fl ooding) of all of Nebraska's rivers and streams. These riparian areas are complex systems with numerous interrelated components (e.g., wetlands, organic matter, sandbars, tree falls, side channels, etc.). Wetlands are an important component of this system by producing invertebrates and other organic matter that provide energy and food to other parts of the streams and rivers. Additionally, these wetlands provide spawning and nursery areas for many types of fi sh, mussels, amphibians, and reptiles, and a home for numerous wildlife species. Historically, there were extensive wetlands associated with the rivers in southeast Nebraska, such as the Little Blue, Big Blue, Nemaha, and Little Nemaha rivers. However, these rivers were highly altered due to channelization and associated down-cutting, and few wetlands remain today. Although some wetlands still occur along all of Nebraska's rivers, this guide focuses on the wetlands associated with the Platte, Missouri, Niobrara, and Elkhorn rivers. These complexes appear to contain the greatest river-associated wetland acreage remaining in the state. The Platte River contains important wetlands throughout its reach; however, in this guide, three segments are singled out for special consideration (Central Platte River, Platte Confl uence and the Lower Platte River). CENTRAL PLATTE RIVER Profi le The Central Platte River (also called the Big Bend Reach) extends approximately 90 miles from Lexington to Chapman. Historically the Platte River was a broad open prairie river with a braided channel and numerous saturated wet meadows adjacent to the river. However, the diversion of approximately 70% of the historic annual fl ows has changed the Central Platte River into a narrower river with a dense band of mixed deciduous woodland and eastern red cedars encroaching on many of the wet meadows. Numerous islands that at one time were open sandbars have

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