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Historical Biogeography of Neotropical Freshwater Fishes最新文献

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Ten. An Ecological Perspective on Diversity and Distributions 十个多样性与分布的生态学视角
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-012
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引用次数: 1
Literature Cited 文献引用
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-022
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引用次数: 0
Fifteen. Northern South America Magdalena and Maracaibo Basins 十五岁。南美洲北部马格达莱纳和马拉开波盆地
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-017
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引用次数: 9
Nine. Continental-Scale Tectonic Controls of Biogeography and Ecology 九个大陆尺度构造对生物地理学和生态学的控制
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-011
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引用次数: 1
Three. Geological Development of Amazon and Orinoco Basins 三。亚马逊河和奥里诺科盆地的地质发展
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-005
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引用次数: 1
Frontmatter
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-fm
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引用次数: 0
Twelve. The Eastern Brazilian Shield 十二年级。巴西东部盾
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-014
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引用次数: 0
Eleven. The Amazon-Paraguay Divide 十一。亚马逊-巴拉圭分水岭
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-013
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引用次数: 0
Fourteen. The Vaupes Arch and Casiquiare Canal Barriers and Passages 十四。Vaupes拱门和Casiquiare运河的屏障和通道
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-016
K. Winemiller, S. Willis
This chapter examines the relationship between the fi sh faunas of the Amazon and Orinoco river basins and distributions of species across the Vaupes Arch region, the major drainage divide in the Llanos region of eastern Colombia and the western limit of the Guiana Shield in Venezuela. Our focus is the differences and similarities in the two faunas and the historical and contemporary geographic and environmental factors that infl uence fi sh distributions, speciation, and adaptation. The subject of this chapter overlaps with several other chapters in this volume; consequently, our discussion will be limited to geological events that occurred after the elevation of the Vaupes Arch approximately 8–10 Ma in the region that encompasses the southern extent of the Colombian Llanos and the Atabapo and Casiquiare subbasins in southwestern Venezuela. The rise of the Vaupes Arch separated the ancient paleo-Amazon-Orinoco River into two separate drainages—the Orinoco fl owing to the north then northeast, and the Amazon fl owing to the east once it had breached the Purús Arch. Discussions of earlier geological events and their infl uence on the fi sh fauna of northern South America appear in other chapters within this volume. In particular, Chapter 7 describes the biogeography of the Neogene, and Chapters 13 and 15 provide detailed descriptions of geological events and their potential infl uence on fi sh distributions in northern South America. These chapters should be consulted for descriptions of events during earlier periods. The Amazon Basin, the largest in the world, covers about 7 million km (about 40% of the area of South America) and has an averaged discharge of nearly 180,000 m/s. The main-stem Amazon River, which is called the Solimões River in Brazil until its junction with the Negro River near the city of Manaus, is estimated to be about 6,700 km long, with approximately 15,000 tributaries and subtributaries—four of which are over 1,600 km long. The Negro River, the huge north-bank tributary, has a mean discharge estimated at 28,000 m/s, which is about 15% of the annual discharge of the Amazon, and which ranks it fi fth among rivers worldwide. Other major tributaries include the Purús, Madeira, Tapajós, Xingu, and Tocantins on the south bank, and the Napo, Japurá, and Trombetas on the north bank. The rivers and streams of the Amazon Basin have highly varied water chemistry (Sioli 1984), ranging from extreme black waters of low pH and conductivity (e.g., Negro) to clear waters with high transparency (e.g., Trombetas), to white waters with neutral pH and low transparency due to high loads of suspended sediments (Napo). In general, rivers draining the Andes in the western region of the basin are white water, and those draining the Guyana and Brazilian Shields are either clear water or black water. Most of the Amazon Basin lies at very low elevation and is covered in tropical forests, with areas of savanna occurring in upland regions of the Guiana Sh
本章考察了亚马逊河和奥里诺科河流域的鱼类动物群与Vaupes Arch地区的物种分布之间的关系,Vaupes Arch地区是哥伦比亚东部Llanos地区和委内瑞拉圭亚那地盾西部边界的主要水系分水岭。我们的重点是两个动物群的差异和相似之处,以及影响鱼类分布、物种形成和适应的历史和当代地理和环境因素。本章的主题与本卷其他几章重叠;因此,我们的讨论将局限于Vaupes Arch抬升后大约8-10 Ma发生的地质事件,该地区包括哥伦比亚Llanos南部地区以及委内瑞拉西南部的Atabapo和Casiquiare子盆地。Vaupes拱门的崛起将古老的古亚马逊河-奥里诺科河分成了两个独立的流域——奥里诺科河向北流,然后向东北流,而亚马逊河在突破Purús拱门后向东流。关于早期地质事件及其对南美洲北部鱼类动物群的影响的讨论出现在本卷的其他章节中。特别是,第7章描述了新近纪的生物地理学,第13章和第15章详细描述了地质事件及其对南美洲北部鱼类分布的潜在影响。这些章节应该参考早期事件的描述。亚马逊盆地是世界上最大的盆地,覆盖约700万公里(约占南美洲面积的40%),平均流量接近18万米/秒。亚马逊河的干流,在巴西被称为Solimões河,直到它与马瑙斯市附近的内格罗河(Negro River)汇合,据估计大约有6700公里长,大约有15000条支流和支流,其中4条超过1600公里长。巨大的北岸支流内格罗河的平均流量估计为28,000米/秒,约占亚马逊河年流量的15%,在世界河流中排名第五。其他主要支流包括位于南岸的Purús、马德拉河、Tapajós、新古河和托坎廷斯河,以及位于北岸的纳波河、日本河和特朗贝塔斯河。亚马逊河流域的河流和溪流具有高度不同的水化学(Sioli 1984),从低pH值和电导率的极端黑色水(例如Negro)到高透明度的清澈水(例如Trombetas),再到pH值中性、高悬浮沉积物负荷导致低透明度的白色水(Napo)。一般来说,流经盆地西部安第斯山脉的河流是白水,而流经圭亚那和巴西盾的河流要么是清水,要么是黑水。亚马逊盆地的大部分地区海拔很低,被热带森林覆盖,热带稀树草原地区出现在北部的圭亚那地盾的高地地区,特别是在东部主干以南的巴西地盾内。这条河的起源是乌卡亚利河的源头,流经秘鲁安第斯山脉的东坡。在离开安第斯山脉向东流向大西洋后,它是一条宽阔蜿蜒的河道,有许多岛屿和侧河道,坡度仅为1.5厘米/公里。奥里诺科河流域全长约100万公里,年平均流量约为3万米/秒,在全球河流中排名第三。据估计,奥里诺科河的主干从委内瑞拉东北部加勒比海沿岸的三角洲到委内瑞拉和巴西边境的帕里马山脉的源头,全长约1500公里。瓜维亚雷河发源于哥伦比亚的安第斯山脉,流经哥伦比亚的大拉诺斯山脉,然后在委内瑞拉的圣费尔南多德阿塔巴波镇附近加入下奥里诺科河,它的河道比上奥里诺科河更大更长,而且与下奥里诺科河的水一样富含沉积物。因此,瓜维亚雷河可以被认为是奥里诺科河的真正干流。在东部和南部,奥里诺科河盆地与圭亚那地盾山脉接壤(图14.1)。在西部,盆地被安第斯山脉的分支与马格达莱纳盆地和马拉开波盆地分开,在北部,它被沿海山脉与小型沿海流域和瓦伦西亚湖盆地分开。下奥里诺科河及其主要支流(如瓜维亚雷河、梅塔河、阿普雷河)大部分流经哥伦比亚和委内瑞拉的大草原,都有宽阔、低坡度的辫状河道。上面的接缝
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引用次数: 8
Two. Major Biogeographic and Phylogenetic Patterns 两个。主要的生物地理和系统发育模式
Pub Date : 2019-12-31 DOI: 10.1525/9780520948501-004
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引用次数: 0
期刊
Historical Biogeography of Neotropical Freshwater Fishes
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