標題: Titlebook: Coastal Marine Ecosystems of Latin America; Ulrich Seeliger,Bj?rn Kjerfve Book 2001 Springer-Verlag Berlin Heidelberg 2001 Bay.Coast.Coral [打印本頁] 作者: 無緣無故 時間: 2025-3-21 19:23
書目名稱Coastal Marine Ecosystems of Latin America影響因子(影響力)
書目名稱Coastal Marine Ecosystems of Latin America影響因子(影響力)學科排名
書目名稱Coastal Marine Ecosystems of Latin America網(wǎng)絡公開度
書目名稱Coastal Marine Ecosystems of Latin America網(wǎng)絡公開度學科排名
書目名稱Coastal Marine Ecosystems of Latin America被引頻次
書目名稱Coastal Marine Ecosystems of Latin America被引頻次學科排名
書目名稱Coastal Marine Ecosystems of Latin America年度引用
書目名稱Coastal Marine Ecosystems of Latin America年度引用學科排名
書目名稱Coastal Marine Ecosystems of Latin America讀者反饋
書目名稱Coastal Marine Ecosystems of Latin America讀者反饋學科排名
作者: 倔強不能 時間: 2025-3-21 20:31 作者: dermatomyositis 時間: 2025-3-22 00:58
The Maracaibo System, Venezuela, de Juana et al. 1980). Within this basin, the Maracaibo System acts as an assemblage of interactive brackish water bodies (>220 km.), comprised of the Gulf of Venezuela, Tablazo Bay and the Maracaibo Strait, which connect Lake Maracaibo in the interior of the basin to the Caribbean Sea (Fig. 3.1). 作者: hankering 時間: 2025-3-22 05:07 作者: 虛假 時間: 2025-3-22 10:55 作者: incarcerate 時間: 2025-3-22 14:58 作者: incarcerate 時間: 2025-3-22 20:08 作者: 披肩 時間: 2025-3-22 21:35
,Baía de Guanabara, Rio De Janeiro, Brazil,politan area. The shallow bay measures 28 km from west to east and 30 km from south to north, has a 131-km perimeter, a mean water volume of 1.87 x 10.m., and 384 km. surface area. The entrance to Baia de Guanabara is only 1.6 km wide (Fig. 8.1). The bay is structurally controlled and has a central 作者: mitral-valve 時間: 2025-3-23 01:31
,The Lagoon Region and Estuary Ecosystem of Cananéia, Brazil,°S, 48°W). A distinctive feature of the estuarine-lagoon complex is the presence of several islands, Cardoso, Cananéia (27 km.), Comprida (70 km.), and Iguape Island. The islands are isolated from the continent by interconnected channels, the Cubat?o and Cananéia Sea and the Trapandé Bay, which are 作者: nascent 時間: 2025-3-23 09:32
,The Subtropical Estuarine Complex of Paranaguá Bay, Brazil,that includes the Iguape-Cananéia Bay system on the southern coast of S?o Paulo State. Rather than being an estuary, Paranaguá Bay (612 km.) is best defined as an estuarine system comprised of two main water bodies, the Paranaguá and Antonina bays (260 km.) and the Laranjeiras and Pinheiros bays (20作者: FLAX 時間: 2025-3-23 10:58
The Convergence Ecosystem in the Southwest Atlantic,rge-scale flow field comprises the south and northward flowing western boundary currents, the Brazil and Malvinas (=Falkland) currents, respectively. The Brazil Current transports warm tropical water (TW) during most of the year towards the southern Brazilian shelf (Garcia 1997), while the coastal b作者: 異端邪說2 時間: 2025-3-23 13:53
The Patos Lagoon Estuary, Brazil,t choked lagoon. About 80% of the lagoon is a freshwater system but at its southern reach (32°S), where the lagoon connects to the Atlantic Ocean, brackish waters and fringing marshes comprise an estuarine ecosystem of approximately 1,000 km. (Fig. 12.1). The estuary performs critical interface func作者: LAY 時間: 2025-3-23 19:39 作者: animated 時間: 2025-3-23 22:19 作者: Nonconformist 時間: 2025-3-24 04:43 作者: 狼群 時間: 2025-3-24 09:17
The Peruvian Coastal Upwelling System, (Guillén 1983), with high productivity originating from equatorial upwelling south of the Galapagos Islands. Peruvian coastal upwelling is peculiar because winds sustain the upwelling process throughout the year (Zuta and Guillén 1970) and the El Ni?o-Southern Oscillation (ENSO) cycle induces disti作者: Malfunction 時間: 2025-3-24 13:05 作者: 金哥占卜者 時間: 2025-3-24 17:32
The Estuary Ecosystem of Buenaventura Bay, Colombia,and NW-SE) on Tertiary consolidated rocky and sedimentary cliffs and on Quaternary mobile sediment platforms (Cantera 1991; Martínez 1993). The NE-SW fault is responsible for uplifting the northern shore of the bay, which is dominated by rocky cliffs, occasional rocky shores and intrusions of sand a作者: 審問,審訊 時間: 2025-3-24 22:08
Reification and the birth of totalitiescent earthquake (6.6 on the Richter scale). The tectonic plate boundary between North and South American lithospheric plates is marked by the Cayman Trench, which bisects the Gulf from northeast to southwest and stretches landward into the Motagua watershed at the Guatemala-Honduras border. As a res作者: 抵押貸款 時間: 2025-3-24 23:11
Awareness-Based Decision-Making Strategy,e open sea (Pannier 1979; Fig. 4.1). The delta itself and the plume are distinct estuarine units; their limits probably depending on interactions brought about by seasonal variations in runoff and intrusion of tidal fronts.作者: Mingle 時間: 2025-3-25 06:30
https://doi.org/10.1007/978-1-4471-2957-8l as reefs and sand banks north of the Catuama and south of the Orange entrance, form a semi-open elongated lagoon-like environment (“inner sea”) which restricts the exchange of water between the Santa Cruz Channel and offshore areas (Medeiros and Kjerfve 1993; Fig. 5.1).作者: 通知 時間: 2025-3-25 09:51 作者: 長處 時間: 2025-3-25 13:39
Interleaving Plans with Dependencies, to the continental slope and on variations in frequency and intensity of NE winds. During strong upwelling, SACW advances beyond the continental slope and invades the shelf to depths of about 50–80 m where is remains until April (mid-fall). The second stage of upwelling, mainly from September to Ma作者: 努力趕上 時間: 2025-3-25 18:34
https://doi.org/10.1007/978-1-4471-1594-6unoff measures 125 m3 s. and peaks in January. Tides are mixed and mainly semidiurnal with a range of 0.7 m, and peak spring tidal currents reach 0.5 m s. inside the bay and 1.6 m s. in the bay entrance. The passage of northward propagating polar fronts occasionally results in strong winds from the 作者: 強有力 時間: 2025-3-25 23:59
https://doi.org/10.1007/978-1-4613-2659-5 ridge plains east of Paranaguá, respectively (Angulo 1992; Angulo and Lessa 1997). An extensive coastal plain surrounds Paranaguá Bay and the upper reaches of the bay originate about 50km inland at the piedmont of the Serra do Mar mountain range. Mangrove swamps and marshes mainly fringe the interi作者: GRAZE 時間: 2025-3-26 03:34 作者: Bernstein-test 時間: 2025-3-26 07:35
Measurements of Charmed Particle Lifetimesh system with an area of about 22,000 km., both depths (5–25 m) and section width increase concomitantly (Fig. 13.1). However, the mixohaline area increases to about 38,000 km. if based on the mean position of the 30 isohaline (Guerrero et al. 1997a,b). The limit between mixohaline waters and conti作者: remission 時間: 2025-3-26 10:04 作者: Inveterate 時間: 2025-3-26 13:15
https://doi.org/10.1007/978-3-319-41045-6tewater from the city of Guayaquil (population of 2.5 million) and to the southeast, the Churute subestuary is influenced by the Churute and Taura Rivers. More than 20 rivers, with a total watershed of 51,230 km., discharge into the Gulf of Guayaquil (Fig. 17.1). The Guayas River, which forms at the作者: GLUT 時間: 2025-3-26 18:52 作者: 貧窮地活 時間: 2025-3-26 22:10 作者: HALO 時間: 2025-3-27 04:18
The Gulf of Honduras,cent earthquake (6.6 on the Richter scale). The tectonic plate boundary between North and South American lithospheric plates is marked by the Cayman Trench, which bisects the Gulf from northeast to southwest and stretches landward into the Motagua watershed at the Guatemala-Honduras border. As a res作者: fetter 時間: 2025-3-27 06:56 作者: Altitude 時間: 2025-3-27 10:26
,The Itamaracá Estuarine Ecosystem, Brazil,l as reefs and sand banks north of the Catuama and south of the Orange entrance, form a semi-open elongated lagoon-like environment (“inner sea”) which restricts the exchange of water between the Santa Cruz Channel and offshore areas (Medeiros and Kjerfve 1993; Fig. 5.1).作者: sparse 時間: 2025-3-27 17:16
The Abrolhos Reefs of Brazil,pe of 0°08′ and the shelf edge at about 70 m. The topography of the inner shelf is smooth and flat while narrow channels and sandbanks are common on the middle and outer shelves. A shallow (Caravelas Channel 15 m) and a deeper (Abrolhos Channel 20–30 m) channel separate the coast from the coastal re作者: anagen 時間: 2025-3-27 20:21
The Cabo Frio Upwelling System, Brazil, to the continental slope and on variations in frequency and intensity of NE winds. During strong upwelling, SACW advances beyond the continental slope and invades the shelf to depths of about 50–80 m where is remains until April (mid-fall). The second stage of upwelling, mainly from September to Ma作者: mediocrity 時間: 2025-3-28 00:23
,Baía de Guanabara, Rio De Janeiro, Brazil,unoff measures 125 m3 s. and peaks in January. Tides are mixed and mainly semidiurnal with a range of 0.7 m, and peak spring tidal currents reach 0.5 m s. inside the bay and 1.6 m s. in the bay entrance. The passage of northward propagating polar fronts occasionally results in strong winds from the 作者: Intruder 時間: 2025-3-28 02:29
,The Subtropical Estuarine Complex of Paranaguá Bay, Brazil, ridge plains east of Paranaguá, respectively (Angulo 1992; Angulo and Lessa 1997). An extensive coastal plain surrounds Paranaguá Bay and the upper reaches of the bay originate about 50km inland at the piedmont of the Serra do Mar mountain range. Mangrove swamps and marshes mainly fringe the interi作者: Melatonin 時間: 2025-3-28 07:00 作者: evaculate 時間: 2025-3-28 10:58
,The Río de la Plata Estuary, Argentina-Uruguay,sh system with an area of about 22,000 km., both depths (5–25 m) and section width increase concomitantly (Fig. 13.1). However, the mixohaline area increases to about 38,000 km. if based on the mean position of the 30 isohaline (Guerrero et al. 1997a,b). The limit between mixohaline waters and conti作者: 浸軟 時間: 2025-3-28 17:22 作者: 溫和女孩 時間: 2025-3-28 18:44
The Gulf of Guayaquil and the Guayas River Estuary, Ecuador,tewater from the city of Guayaquil (population of 2.5 million) and to the southeast, the Churute subestuary is influenced by the Churute and Taura Rivers. More than 20 rivers, with a total watershed of 51,230 km., discharge into the Gulf of Guayaquil (Fig. 17.1). The Guayas River, which forms at the作者: Obloquy 時間: 2025-3-29 02:37
The Estuary Ecosystem of Buenaventura Bay, Colombia,(Lobo-Guerrero 1993). The addition of sediments and their transport by rivers and tides also causes their continuous deposition in the navigation channel and leads to a prograding southern coast (CAE 1995; Univalle 1997).作者: 勤勉 時間: 2025-3-29 04:58 作者: 強行引入 時間: 2025-3-29 09:54 作者: 典型 時間: 2025-3-29 13:17
0070-8356 examines management issues.Includes supplementary material:Coastal and marine ecosystems, some severely degraded, other still pristine, control rich resources of inshore environments and coastal seas of Latin America‘s Pacific and Atlantic margins. Conflicts between the needs of the region‘s nation作者: gorgeous 時間: 2025-3-29 18:41
The Standard Model of Particle Physicssand flats at the mouth of rivers in south-central Chile between 38°S and 42°S and with rocky peninsulas in the extreme north (19–30°S; Fig. 15.1). Seasonal cycles of beach sand erosion and accretion are typical. During erosion, beaches have concave profiles with coarser grained sand than during accretion periods, when profiles are convex.作者: 音樂等 時間: 2025-3-29 21:01 作者: CAND 時間: 2025-3-30 03:36 作者: 小口啜飲 時間: 2025-3-30 08:02 作者: 不連貫 時間: 2025-3-30 10:11
https://doi.org/10.1007/978-3-319-41045-6nct interannual ecosystem variability. The coastal upwelling system, which hardly comprises 0.02% of the total ocean surface, is of great significance because it determines the enormous productivity of Peruvian coastal waters, representing almost 20% of the world’s landings of industrial fish.作者: 巨頭 時間: 2025-3-30 14:14
The Maracaibo System, Venezuela,Eustatic sea level changes during the Holocene have induced either fresh or brackish water conditions in the lake. After the last transgression (about 9,000 years ..), when sea levels were about 20 m above present levels, numerous islands and bars were formed at the mouth of the estuary.作者: 恃強凌弱 時間: 2025-3-30 16:57
,The Lagoon Region and Estuary Ecosystem of Cananéia, Brazil,1–3 km wide and up to 20 m deep (mean depth 6 m). The backwaters and small rivers are shallower and characteristically fringed by mangrove vegetation. The system connects with the Atlantic Ocean through channels at the northern (Barra de Icaparra) and southern (Barra de Cananéia) end of Comprida Island (Tessler and Souza 1998; Fig. 9.1).作者: Optimum 時間: 2025-3-31 00:27 作者: PACT 時間: 2025-3-31 01:11
Book 2001ngs, biotic components and structure of the system, considers trophic processes and energy flow, evaluates the modifying influence of natural and human perturbations, and suggests management needs. Although the focus of the book is on basic ecological research, the results have application for coastal managers.作者: 形上升才刺激 時間: 2025-3-31 06:05
The nature and meaning of the totalistins and alluvial fans characterize the Atlantic coastline. Today, approximately 93% of South America’s drainage is to the Caribbean and the Atlantic away from the Andes and provides the world’s best example of present-day continent-scale drainage control by plate tectonics (Inman and Nordstrom 1971; Hoorn et al. 1995; Potter 1997).作者: Decimate 時間: 2025-3-31 10:27 作者: GUISE 時間: 2025-3-31 17:03 作者: EXPEL 時間: 2025-3-31 18:53
The Patos Lagoon Estuary, Brazil,-chemical characteristics which control ecological processes and vital habitats for the successful reproduction and/or growth of many commercially important marine species which visit the estuary periodically.作者: Urgency 時間: 2025-4-1 01:13
The nature and meaning of the totalistrine ecosystems of South America. The continent’s Phanerozoic tectonic history is dominated by its separation from Africa and the Mid-Miocene uplift of the Andes. Tectonically, South America is divided into two parts, the Andean chain to the west and a vast stable platform to the east, consisting of作者: 紅潤 時間: 2025-4-1 03:01
Reification and the birth of totalitiesclusive economic zones of Belize, Guatemala, and Honduras. For purposes of this paper, the Gulf extends from Gladden Spit (16.5° N, 88° W) on the Belize barrier reef to Punta Sal (15.9° N, 87.6° W) on the north coast of Honduras, including Bahia de Amatique and the entire Caribbean coast of Guatemal作者: 譏笑 時間: 2025-4-1 07:35
The nature and meaning of the totalist de Juana et al. 1980). Within this basin, the Maracaibo System acts as an assemblage of interactive brackish water bodies (>220 km.), comprised of the Gulf of Venezuela, Tablazo Bay and the Maracaibo Strait, which connect Lake Maracaibo in the interior of the basin to the Caribbean Sea (Fig. 3.1). 作者: genuine 時間: 2025-4-1 12:58
Awareness-Based Decision-Making Strategy,the Sierra Parima and Sierra Unturan near Brazil and the Atlantic Ocean, the Orinoco drains more than 2,000 rivers (Depetris and Paolini 1991; Bonilla et al. 1993; Cressa et al. 1993). The distinctive triangular-shaped Orinoco Delta (20,000 km.) includes a cluster of ecosystems (Pannier 1979; Lewis 作者: 樂章 時間: 2025-4-1 16:58
https://doi.org/10.1007/978-1-4471-2957-8ult which gave origin to the Santa Cruz Channel was flooded by seawater and connected with the South Atlantic Ocean by the Catuama and Orange entrance (Fig. 5.1). Offshore regions typically have a series of two or three parallel sandstone reefs (20–60 m wide) which consist of cemented sand (20–80% o作者: 描述 時間: 2025-4-1 21:41
https://doi.org/10.1007/978-3-319-41192-7 reports on Abrolhos coral reefs are those from the Darwin visit to the Abrolhos Archipelago; however, it was the Thayer Expedition led by Louis Agassiz that produced the seminal work with a first detailed description of coral zonation on the reefs (Hartt 1870). The Abrolhos reef ecosystem, which oc作者: 向外供接觸 時間: 2025-4-2 02:10
