Aman Iman: Resilient Customs, Community Water Management, and Dry Futures in Anounizme, Morocco

This project explores how Anounizme, a village in southeastern Morocco, interacts with water. I was particularly curious about how traditional community management systems operate in the context of drought. I argue that the customary management system exhibits resiliency like it has in the face of Arabization, colonization, exploitative industry, and land privatization. It is capable of adapting to drought because it is more than a management system; it is a part of culture engrained as custom. Customs have porous boundaries, allowing a space for old aspects of culture to interact with both emerging aspects of culture and external pressures. I draw upon existing scholarship surrounding the commons, customs, khettara, and community resource management in the region. I turn to semi-structured interviews and participant observation in Anounizme to better understand this scholarship in the context of drought and desertification. This research takes unique relevance as there is little field-based research in the region, and it explores customs and community management in the framework of water scarcity

Expanded oxygen minimum zones during the late Paleocene-early Eocene:Hints from multiproxy comparison and ocean modeling

Anthropogenic warming could well drive depletion of oceanic oxygen in the future. Important insight into the relationship between de-oxygenation and warming can be gleaned from the geological record, but evidence is limited because few ocean oxygenation records are available for past greenhouse climate conditions. We use I/Ca in benthic foraminifera to reconstruct late Paleocene through early Eocene bottom and pore-water redox conditions in the South Atlantic and Southern Indian Oceans, and compare our results with those derived from Mn speciation and the Ce anomaly in fish teeth. We conclude that waters with lower oxygen concentrations were widespread at intermediate depths (1.5-2 km), whereas bottom waters were more oxygenated at the deepest site, in the Southeast Atlantic Ocean (>3 km). Epifaunal benthic foraminiferal I/Ca values were higher in the late Paleocene, especially at low oxygen sites, than at well-oxygenated modern sites, indicate higher seawater total iodine concentrations in the late Paleocene than today. The proxy-based bottom water oxygenation pattern agrees with the site-to-site O2 gradient as simulated in a comprehensive climate model (CCSM3), but the simulated absolute dissolved O2 values are low (<~35 µmol/kg), while higher O2 values (~60-100 µmol/kg) were obtained in an Earth system model (cGENIE). Multi-proxy data together with improvements in boundary conditions and model parameterization are necessary if the details of past oceanographic oxygenation are to be resolved