Lake Chad flooded savanna
Lake Chad flooded savanna
The Lake Chad flooded savanna is an Afrotropic flooded-grassland ecoregion centered on the basin of Lake Chad, straddling the borders of Cameroon, Chad, Niger, and Nigeria. It is a mosaic of open water, papyrus and reed beds, seasonally flooded grasslands, and Acacia woodland: the southern lake supports Cyperus papyrus, Phragmites mauritianus, and Vossia cuspidata, the saltier north favors Phragmites australis and Typha, and Acacia seyal is the predominant tree of the drier margins. The climate is tropical and dry, with around 320 mm of rainfall a year concentrated in a June-to-October wet season, so the lake depends heavily on the Chari and Logone Rivers rather than on local rain. It is a critical refuge for waterbirds, hosting many wetland species and large numbers of Palearctic migrants such as ruff, with the secretary bird serving as its flagship species, though the lake has shrunk dramatically in recent decades under pressure from drought, water diversion, and agriculture. For gardeners, the region's native flora includes ornamental wetland and dryland genera grown elsewhere, notably papyrus (Cyperus) and Acacia.
RESOLVE 72
Afrotropic
12,396 sq mi
Flooded Grasslands & Savannas
Type de paysage
Flooded Grasslands & Savannas
Région végétale
Afrotropic
Empreinte de la région
12,396 sq mi
Pression sur l'habitat
Nature Could Recover (Dinerstein NNH 3)
Sourcing et entretien
Sponsorisé
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Utilisez ceci comme schéma général de plantation pour la région : Grasslands and savannas subject to seasonal or year-round flooding, including large wetland complexes. Exceptionally productive, they concentrate waterbirds and aquatic life. Pour vos décisions de jardin, associez ce contexte à la liste de plantes ci-dessous, puis affinez selon les contraintes de lumière, d'eau, de sol et de taille adulte de votre site.
Range & origins
Repère placé à l’intérieur du polygone RESOLVE 2017 à 13.3°N, 14.1°E.
La région à travers le temps
Empreinte moderne
RESOLVE 2017 cartographie 12,396 sq mi
Cette limite est une empreinte écologique moderne pour Lake Chad flooded savanna, et non une ligne permanente sur la planète. Elle est utile pour le contexte actuel des plantes et de la faune car elle suit des schémas récurrents de végétation, de climat, de relief et de perturbations.
Pourquoi ici
Conditions de flooded grasslands & savannas
La région se situe dans le règne Afrotropic et est classée comme flooded grasslands & savannas. L'altitude, l'humidité, le feu, les sols, les côtes et l'utilisation humaine des terres peuvent tous rendre le paysage réel plus varié qu'une seule couleur de carte ne le laisse penser.
Pression du changement
Nature Could Recover
Plotwright affiche ceci comme l'empreinte RESOLVE actuelle. Au fil des décennies ou des siècles, le réchauffement, les perturbations, les espèces envahissantes, l'utilisation des terres et la restauration peuvent déplacer la bordure vivante d'une région même lorsque la carte de référence reste fixe.
Régions de plantation similaires
Parcourez d'autres régions au rythme similaire d'étés chauds et secs. Leurs listes de plantes peuvent suggérer des espèces et des combinaisons à comparer.
RESOLVE 69 - Afrotropic
East African halophytics
The East African halophytics ecoregion covers the saline soda lakes of the eastern arm of the Great Rift Valley, spanning northern Tanzania and southern Kenya, and takes in Lake Natron, Lake Eyasi, and Lake Manyara on the Tanzanian side along with Lake Magadi in Kenya. Resting on volcanic lava and ash that weather into deep, sodium-rich soils, the lakes are largely devoid of rooted (macrophytic) vegetation; instead they teem with blue-green algae, chiefly Spirulina, while only a few salt-loving halophytic plants persist on the alkaline soils fringing the water. The climate is semi-arid, with erratic rainfall concentrated between December and May, a long dry season, and daytime temperatures that frequently climb above 40 degrees Celsius alongside high evaporation. Despite waters so hot and alkaline that most life is excluded, the ecoregion is globally important for the lesser flamingo, its flagship species, with Lake Natron serving as the single most important breeding site for the bird, and it also shelters endemic salt-tolerant alkaline tilapia in its hot-spring margins.
Flooded Grasslands & Savannas
Zones 12b-13a
+3.9°F d’ici 2070
1,464 sq mi
Niveau NNH 3
RESOLVE 70 - Afrotropic
Etosha Pan halophytics
The Etosha Pan halophytics ecoregion lies entirely within Etosha National Park in northern Namibia, encompassing a vast saline depression of roughly 4,850 square kilometers that forms part of the Cuvelai-Etosha Basin and is the remnant of a large inland Pliocene lake. This is the largest pan system in Namibia, mostly dry cracked clay that floods with a thin, heavily salted sheet of water after good rains. Vegetation is sparse and salt-tolerant: the pan surface is colonized by grasses such as Sporobolus spicatus that flush quickly after rain, while dense mopane woodland frames the surrounding margins. The climate is harsh and strongly seasonal, with a mean annual rainfall near 430 millimeters falling mostly in late summer, three distinct seasons (hot and wet, cool and dry, hot and dry), and temperatures swinging from below freezing in winter to over 45 degrees Celsius in summer. The pan is a Ramsar wetland of international importance and a crucial breeding ground, drawing up to 1.1 million flamingos in flood years alongside its flagship great white pelican, and the park supports one of the largest black rhino populations in the world.
Flooded Grasslands & Savannas
Zones 12a
+4.4°F d’ici 2070
2,978 sq mi
Niveau NNH 1
RESOLVE 71 - Afrotropic
Inner Niger Delta flooded savanna
The Inner Niger Delta flooded savanna occupies the vast inland delta of the Niger River in central Mali, a green oasis set within the semi-arid Sahel just south of the Sahara between the towns of Djenné and Tombouctou. It is the largest inland wetland in West Africa and the second largest on the continent after Botswana's Okavango Delta. Its defining rhythm is seasonal flooding: rains falling on Guinea's Fouta Djalon highlands from roughly May to September send a flood surge that reaches the delta around October, expanding the wetland dramatically before it contracts in the hot dry months. Characteristic plants include bourgou (Echinochloa stagnina) and beardgrass (Andropogon gayanus) on the floodplains, flooded forests of Acacia kirkii with some Ziziphus mauritiana, and stands of doum palm (Hyphaene thebaica) and African fan palm (Borassus aethiopum). The delta is a globally important bird wintering ground, drawing over a million waterbirds in wet years including hundreds of thousands of garganey and northern pintail, with the Nile monitor as its flagship species and several Ramsar sites recognizing its value. Gardeners in hot, strongly seasonal climates may know the heat- and flood-tolerant doum and Borassus fan palms as striking architectural ornamentals native to this region.
Flooded Grasslands & Savannas
Zones 12b-13a
+3.8°F d’ici 2070
17,771 sq mi
Niveau NNH 1
RESOLVE 73 - Afrotropic
Makgadikgadi halophytics
The Makgadikgadi Halophytics ecoregion occupies the vast Makgadikgadi Pan complex of northeastern Botswana, a salt-encrusted basin southeast of the Okavango Delta and ringed by the Kalahari that holds two major pans, Ntwetwe and Sua, along with many smaller ones. It is the remnant of an enormous ancient lake that dried up tens of thousands of years ago, leaving a flat expanse of soda-saturated clay fed seasonally by the Boteti and Nata rivers. The pan floors are almost devoid of higher plants apart from a thin film of blue-green algae, while their wetter fringes grade into salt marshes and grasslands where salt-tolerant grasses take hold, and the surrounding savanna carries scattered baobabs. The climate is semi-arid, with rain falling mainly as summer thunderstorms and droughts recurring in roughly seven-year cycles. Sua Pan is the most important breeding site in Africa for the greater flamingo, the ecoregion's flagship species, and supports southern Africa's largest breeding population of lesser flamingo, with much of the region protected within Makgadikgadi and Nxai Pan National Park.
Flooded Grasslands & Savannas
Zones 11b-12b
+4.5°F d’ici 2070
6,810 sq mi
Niveau NNH 2
RESOLVE 74 - Afrotropic
Sudd flooded grasslands
The Sudd flooded grasslands form one of Africa's largest wetlands, spreading across the White Nile floodplain in South Sudan with a marginal reach into Ethiopia. Vegetation is arranged in zones tied to flood depth: dense stands of papyrus (Cyperus papyrus), reeds such as Phragmites, and cattail (Typha) dominate the permanently wet channels, while floating-rooted hippo grass (Vossia cuspidata) and seasonally flooded swards of wild rice and Echinochloa grasses occupy the shallower margins. The climate is hot and strongly seasonal, with rains falling roughly April to September under the migrating Intertropical Convergence Zone and the wetter south receiving more than the drier north. The Sudd is a biodiversity stronghold, supporting over 400 bird species and the world's largest population of the shoebill, and serving as the stage for one of Earth's greatest mammal migrations as white-eared kob, tiang, and Mongalla gazelle move across the plains. Gardeners may recognize papyrus, native here, as a familiar ornamental water-garden sedge.
Flooded Grasslands & Savannas
Zones 13b
+3.8°F d’ici 2070
72,937 sq mi
Niveau NNH 3
RESOLVE 75 - Afrotropic
Zambezian coastal flooded savanna
The Zambezian coastal flooded savanna is restricted to the coastal lowlands of Mozambique, comprising the floodplain deltas of the Zambezi, Pungwe, Buzi, and Save rivers, with the vast Zambezi delta stretching nearly 200 km along the Indian Ocean coast and reaching up to 120 km inland. It is a mosaic of seasonally flooded grasslands and savanna interwoven with mixed freshwater swamp forests, whose plant communities shift with soil type and flooding duration: reed swamps of Phragmites and Typha, grasses such as Hyparrhenia, Ischaemum, and Setaria, and scattered trees and palms including Parinari, Uapaca, Syzygium, and Borassus. Rainfall is strongly seasonal, with most of the roughly 800 to 1,400 mm falling between October and March, and the river-driven flood pulse governs which habitats develop. The wetlands hold the highest concentration of waterbirds in Mozambique and are a stronghold for the wattled crane, the ecoregion's flagship species, with portions protected within the Marromeu National Reserve and Gorongosa National Park. For gardeners, several striking palms are native here, among them the wild date palm (Phoenix reclinata) and the fan palm Hyphaene coriacea.
Flooded Grasslands & Savannas
Zones 13a-13b
+3.7°F d’ici 2070
7,501 sq mi
Niveau NNH 3
Sources et citations
Citer cette page
Pour les plans de cours, articles ou notes de plantation régionales qui utilisent cette page Plotwright. Pour citer le cadre d'écorégions sous-jacent ou un profil éditorial spécifique, utilisez les fiches de sources ci-dessous.
Plotwright. (n.d.). Lake Chad flooded savanna (Lake Chad flooded savanna). Retrieved 2026, June 24, from https://plotwright.com/regions/resolve-72
Sources pour cette région
Cette page cite d'abord Plotwright pour la vue compilée, puis répertorie les pages sources du cadre, du climat et de l'éditorial en amont afin que les lecteurs puissent citer directement le matériel d'origine.
RESOLVE 2017 Terrestrial Ecoregions (Dinerstein et al.)
Cadre principal des écorégions
Étaye 4 champs
Identifiant RESOLVE
Biome + règne
Superficie
Palier NNH
Wikipedia
Wikimedia Foundation
Étaye 1 champ
Vérification croisée du résumé