Cloud forests of the Orinoco River Basin (Colombia): Variation in vegetation and soil macrofauna composition along the hydrometeorological gradient. (9th February 2023)

• Record Type: Journal Article
• Authors: Ramírez, Beatriz H.; Cortés‐B, Rocío; Pinzón, Olga Patricia; Gómez, Laura; Jacquin, Santiago; Hernández, Eduardo; Quimbayo, Luz Angélica; Bogotá‐A, Raúl Giovanni
• Is Part Of: Biotropica. Volume 55:Number 2(2023)
• Page Start: 489
• Page End: 503
• Publication Date: 2023-02-09
• Subjects: Casanare -- Chámeza -- climate change -- indicator taxa -- mountain ecosystem; Biotic communities -- Tropics -- Periodicals; Applied ecology -- Tropics -- Periodicals; Biology -- Tropics -- Periodicals; 577.80913
• DOI: 10.1111/btp.13203
• Languages: English
• ISSNs: 0006-3606

Abstract

Abstract: Tropical montane cloud forests (TMCF) in the Orinoco River Basin are vulnerable to climate and regional land‐use changes. These changes will force TMCF to migrate upwards, affecting biodiversity conservation and water flow regulation. Here, we evaluate how vegetation and soil macrofauna composition vary along the hydrometeorological gradient driven by an increase in fog incidence with elevation. Vegetation data were collected for all individuals with a diameter at breast height (DBH) > 5 cm in four vegetation plots (5 × 50 m; total: 0.1 ha) every 100 m in altitude between 1700 and 2200 m a.s.l. From each plot, we obtained three soil monoliths from the organic layer and three from the mineral horizon, and manually extracted their soil macrofauna. For these groups, we describe: (1) their compositional changes along the hydrometeorological gradient employing ordination analyses techniques and (2) the relation of the composition changes between vegetation and soil macrofauna communities using a symmetrical co‐correspondence analysis. Our results show that the vegetation morphospecies composition and soil macrofauna‐order composition vary significantly with the hydrometeorological gradient along elevation. The co‐correspondence between vegetation and soil macrofauna reveals a shared breakpoint above the 2000 m a.s.l., where fog is more persistent. Furthermore, we identified eight indicator vegetation species and two soil macrofauna orders associated with specific elevations. These results suggest that under a climate‐change‐driven fog lift, the TMCF of the Orinoco River Basin will be displaced. Moreover, this study provides a baseline to monitor such displacement. Abstract in Spanish is available with online material. Abstract : Our results show that the vegetation morphospecies composition and soil macrofauna‐order composition vary significantly with the hydrometeorological gradient along elevation. The co‐correspondence between vegetation and soil macrofauna reveals a shared breakpoint above the 2000 m a.s.l., where fog is more persistent. We identified eight indicator vegetation species and two soil macrofauna orders. Abstract: Tropical montane cloud forests (TMCF) in the Orinoco River Basin are vulnerable to climate and regional land‐use changes. These changes will force TMCF to migrate upwards, affecting biodiversity conservation and water flow regulation. Here, we evaluate how vegetation and soil macrofauna composition vary along the hydrometeorological gradient driven by an increase in fog incidence with elevation. Vegetation data were collected for all individuals with a diameter at breast height (DBH) > 5 cm in four vegetation plots (5 × 50 m; total: 0.1 ha) every 100 m in altitude between 1700 and 2200 m a.s.l. From each plot, we obtained three soil monoliths from the organic layer and three from the mineral horizon, and manually extracted their soil macrofauna. For these groups, we describe: (1) their compositional changes along the hydrometeorological gradient employing ordination analyses techniques and (2) the relation of the composition changes between vegetation and soil macrofauna communities using a symmetrical co‐correspondence analysis. Our results show that the vegetation morphospecies composition and soil macrofauna‐order composition vary significantly with the hydrometeorological gradient along elevation. The co‐correspondence between vegetation and soil macrofauna reveals a shared breakpoint above the 2000 m a.s.l., where fog is more persistent. Furthermore, we identified eight indicator vegetation species and two soil macrofauna orders associated with specific elevations. These results suggest that under a climate‐change‐driven fog lift, the TMCF of the Orinoco River Basin will be displaced. Moreover, this study provides a baseline to monitor such displacement.