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| - | The Paramo de Sumapaz is an extremely biodiverse grassland-peatland ecosystem at high altitude in the xxx mountains. The Paramo experiences low intensity rainfall and frequent fog, which the vegetation captures and stores. Soil moisture is also kept high by the hydraulic connectivity of the soil and acts as a key regulator of surface runoff production. At the foot of the hillslopes and the bottom of valleys, organic rich soils and cushion plants maintain saturated conditions. On hillslopes, freely draining soils and tussock grass conduce lateral flow and connectivity with the channel network, as well as both deep soil horizons and shallow groundwater which drain via riparian areas into streams. | ||
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| - | The densely populated area of Bogota depend on the surface and shallow subsurface water of the Paramo as a main source for human consumption, | ||
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| - | Citizen science and participatory monitoring has been found to be an effective tool for generating locally relevant knowledge on the function, use, degradation and management of the Paramo, as well as remote sensing. | ||
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| - | Extremeley biodiverse | ||
| - | High altitude, compared to settlements, | ||
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| - | Grassland-peatland biome | ||
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| - | Used for livelihoods and wellbeing - intensive livestock, cultivation and land management practices negatively affect Paramos' | ||
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| - | Spiritual landscapes | ||
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| - | Main source of water – crop cultivation, | ||
| - | ‘unique source of untapped genetic diversity’ | ||
| - | Functioning of paramo is not fully understood – without knowledge, interventions designed for sustainability could be ineffective or detrimental | ||
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| - | Capture store atmospheric water | ||
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| - | Socio-ecological systems shaped by human populations | ||
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| - | Densely populated areas depend on surface and shallow subsurface water for human consumption, | ||
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| - | Surface water is particularly succeptible to the potential changes in land use and land cover – leading to lower water availability and quality | ||
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| - | HIGH LEVEL OF FRAGMENTATION – historic dynamic landscape, changes in isolation and connectivity defined by complex topography | ||
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| - | Surrounded by low intensity rainfall and frequent fog | ||
| - | Hydrological response of paramo is strongly related to soil conditions - hydraulic conductivity of soil keeps soil moisture high - Soils are important regulators of runoff production (Harden 2006) | ||
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| - | Organic rich soils are at foot of hill slopes and bottom of valleys- covered in cushion plants, saturated conditions | ||
| - | Freely drainig soils on hillslopes under cover of tussock grass | ||
| - | In periods of heavier rainfall, contributing areas of paramo to run off ecxpands and increases connectivity with lateral flow from hillslopes. | ||
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| - | Framing the Páramo through Latour’s Actor–Network Theory reveals its role within a network of non-human actors that intertwines social, political, and ecological dimensions (Latour, | ||
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| - | The Páramo also extends into the spiritual and cultural sphere, where it is regarded as a sacred landscape that sustains both ecological and social life. Within many Andean communities, | ||
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| - | __Bibliography__ | ||
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| - | Baruffol, M. (no date) Andean ‘water sponges’: The role of plants in water supply, Kew. Available at: [[https:// | ||
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| - | https:// | ||
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| - | UK CENTRE FOR ECOLOGY AND HYDROLOGY https:// | ||
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