TY - JOUR
T1 - Late Quaternary climate change, relict populations and present-day refugia in the northern Atacama Desert
T2 - A case study from Quebrada La Higuera (18° S)
AU - Mujica, María Isabel
AU - Latorre, Claudio
AU - Maldonado, Antonio
AU - González-Silvestre, Leticia
AU - Pinto, Raquel
AU - de Pol-Holz, Ricardo
AU - Santoro, Calogero M.
N1 - Publisher Copyright:
© 2014 John Wiley & Sons Ltd.
PY - 2015/1/1
Y1 - 2015/1/1
N2 - Aim: In deserts, past climate change (and particularly past rainfall variability) plays a large role in explaining current plant species distributions. We ask which species were most and which were least affected by changes in rainfall during the late Quaternary in northernmost Chile. Location: Quebrada La Higuera (QLH; 18° S), a shallow canyon that cuts east-west through the western Andean precordillera of northern Chile, connecting the Altiplano with the hyperarid Atacama Desert. Methods: We collected and dated 22 rodent middens from elevations of 3100-3500 m in QLH. These were analysed for identifiable plant macrofossils and pollen. We also measured chinchilla rat (Abrocoma cinerea) faecal pellets in the youngest middens to explore how they relate to past ecological and climatic change. Results: The three oldest middens dated to more than 37 ka (thousand calibrated 14C years), four middens dated to 14.4-11.6 ka, and fifteen middens spanned the last 650 years. During all the intervals examined, extralocal species (those found today at higher elevations and indicative of positive rainfall anomalies) were present at our midden sites. In the youngest interval, Parastrephia pollen (indicating increased rainfall) increased abruptly at ad 1760 and remained high until the mid-1800s. This increase was also seen in our faecal pellet record. Main conclusions: Extralocal species were prevalent in late Pleistocene middens at lower elevations when the climate was wetter. When combined with other regional midden records, we postulate that many species found today in the Altiplano were displaced to lower elevations during the late Pleistocene. The recent large-scale mortality documented among arboreal cactus populations along the present upper margins of the Atacama suggests that these are relict populations that are likely to have flourished during a wetter period in the early 1800s.
AB - Aim: In deserts, past climate change (and particularly past rainfall variability) plays a large role in explaining current plant species distributions. We ask which species were most and which were least affected by changes in rainfall during the late Quaternary in northernmost Chile. Location: Quebrada La Higuera (QLH; 18° S), a shallow canyon that cuts east-west through the western Andean precordillera of northern Chile, connecting the Altiplano with the hyperarid Atacama Desert. Methods: We collected and dated 22 rodent middens from elevations of 3100-3500 m in QLH. These were analysed for identifiable plant macrofossils and pollen. We also measured chinchilla rat (Abrocoma cinerea) faecal pellets in the youngest middens to explore how they relate to past ecological and climatic change. Results: The three oldest middens dated to more than 37 ka (thousand calibrated 14C years), four middens dated to 14.4-11.6 ka, and fifteen middens spanned the last 650 years. During all the intervals examined, extralocal species (those found today at higher elevations and indicative of positive rainfall anomalies) were present at our midden sites. In the youngest interval, Parastrephia pollen (indicating increased rainfall) increased abruptly at ad 1760 and remained high until the mid-1800s. This increase was also seen in our faecal pellet record. Main conclusions: Extralocal species were prevalent in late Pleistocene middens at lower elevations when the climate was wetter. When combined with other regional midden records, we postulate that many species found today in the Altiplano were displaced to lower elevations during the late Pleistocene. The recent large-scale mortality documented among arboreal cactus populations along the present upper margins of the Atacama suggests that these are relict populations that are likely to have flourished during a wetter period in the early 1800s.
KW - Altiplano
KW - Atacama Desert
KW - Central Andes
KW - Late Quaternary
KW - Pluvial events
KW - Refugia
KW - Relict populations
KW - Rodent middens
UR - https://www.scopus.com/pages/publications/84915768030
U2 - 10.1111/jbi.12383
DO - 10.1111/jbi.12383
M3 - Article
AN - SCOPUS:84915768030
SN - 0305-0270
VL - 42
SP - 76
EP - 88
JO - Journal of Biogeography
JF - Journal of Biogeography
IS - 1
ER -