Rachel Lamb earned her PhD in Geographical Sciences at the University of Maryland College Park in Spring 2021. Her research centers on the applications of NASA Carbon Monitoring System forest carbon science to advance strategic climate mitigation planning with co-benefits for biodiversity and human livelihoods. Since 2020, she has lead the Campus Forest Carbon project, helping the University of Maryland better incorporate forest carbon science into their Climate Action Plan and Greenhouse Gas Inventory.
Over the past decade, Rachel has worked for numerous agencies and organizations, including the Texas Commission on Environmental Quality, A Rocha Peru, National Socio-Ecological Synthesis Research Center (SESYNC), Society for Conservation Biology, and the U.S. Environmental Protection Agency. During the summers, she teaches Environmental Law and Policy and Land Resources Policy at the Au Sable Institute of Environmental Studies in Michigan as an Associate Professor. Rachel also supports several faith-based NGOs, including as Senior Advisor to YECA and as a member of the A Rocha USA Board of Directors.
Smithville is a community on Maryland’s Eastern Shore, on the edge of the Blackwater National Wildlife Refuge. A century ago, Smithville had more than 100 residents. Today, it has four, in two homes: an elderly couple, and one elderly woman and her son, who cares for her.
Leone Yisrael is a cephalopod-loving scuba diver, cook, and loves to try new activities. She conducts genetic analysis and fieldwork at the Smithsonian Environmental Research Center through the Coastal Disease Ecology Lab.
Oyster aquaculture is a rapidly growing industry in Maryland’s Chesapeake waters which stimulates economic activity and may provide a host of ecosystem benefits. A potential concern associated with the intensification of the oyster aquaculture is the local production and accumulation of oyster biodeposits, which can lead to a porewater sulfide accumulation and declining bioturbation, symptoms of declining ecosystem function. Sulfide is naturally removed from the seafloor by the interactions between bioturbating infauna and sulfide oxidizing bacteria.