Sand Island, one of the first islands on the atoll to have successfully eradicated coconut palms, which were quickly replaced by a healthy Pisonia forest with abundant shorebird life.
Miriam Jones, Ph.D.
I use a range of proxies (plant macrofossils, pollen, charcoal, stable isotopes) to interpret climate and landscape change over centennial to millennial timescales. Current topics include responses to abrupt permafrost thaw, sea-level rise, sea-ice retreat, and centennial-scale land-use change.
Education and Certifications
Columbia University, PhD, 2008
Columbia University, MPhil, 2006
Columbia University, M. A., 2005
Barnard College, A.B., 2002, Magna Cum Laude
Science and Products
Reconstructing Vegetation and Climate Histories on Palmyra Atoll to Assist with Climate-Smart Adaptation
Holocene and Modern Drivers of Wetland Change
Wetlands in the Quaternary
Wetlands in the Quaternary Project
Charcoal data from four sites in Great Dismal Swamp National Wildlife Refuge - August 2022
Radiocarbon dates, charcoal, and polycyclic aromatic hydrocarbon (PAH) data from Great Dismal Swamp Sites GDS-519 and GDS-520
Carbon budget assessment of tidal freshwater forested wetland and oligohaline marsh ecosystems along the Waccamaw and Savannah rivers, U.S.A. (2005-2016)
Sand Island, one of the first islands on the atoll to have successfully eradicated coconut palms, which were quickly replaced by a healthy Pisonia forest with abundant shorebird life.
A view of the shoreline with palm trees above bright blue water in the Western Lagoon, Palmyra Atoll.
A view of the shoreline with palm trees above bright blue water in the Western Lagoon, Palmyra Atoll.
Aerial view of the Palmyra Atoll, looking west. The forested island is surrounded by blue water.
Aerial view of the Palmyra Atoll, looking west. The forested island is surrounded by blue water.
A recently treated stand of coconut palms, standing and dead, which will naturally convert back to Pisonia forest, on Palmyra Atoll.
A recently treated stand of coconut palms, standing and dead, which will naturally convert back to Pisonia forest, on Palmyra Atoll.
A view of the sandy north shore of Palmyra Atoll, with a forested edge. Recently killed coconut palm trunks poke out of the forested area.
A view of the sandy north shore of Palmyra Atoll, with a forested edge. Recently killed coconut palm trunks poke out of the forested area.
A White Tern and a Red-Footed Booby share some shade under a tree. The White Tern flies while the Booby sits below.
A White Tern and a Red-Footed Booby share some shade under a tree. The White Tern flies while the Booby sits below.
Calm, clear and bright blue waters of a small shoreline lagoon on Palmyra Atoll.
Calm, clear and bright blue waters of a small shoreline lagoon on Palmyra Atoll.
Crystal clear, turquoise waters surrounding a palm-lined beach on Palmyra Atoll.
Crystal clear, turquoise waters surrounding a palm-lined beach on Palmyra Atoll.
Calm, blue waters surround Palmyra Atoll. This view takes in the ocean scenery with a partial glimpse of lush green coastal vegetation on the landward side.
Calm, blue waters surround Palmyra Atoll. This view takes in the ocean scenery with a partial glimpse of lush green coastal vegetation on the landward side.
Driftwood lays partially submerged in clear blue water on sandy shore of Palmyra Atoll.
Driftwood lays partially submerged in clear blue water on sandy shore of Palmyra Atoll.
Photograph of Lake Drummond, which is located within the Great Dismal Swamp in Virginia. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Photograph of Lake Drummond, which is located within the Great Dismal Swamp in Virginia. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Photograph of the Great Dismal Swamp in Virginia.
Photograph of the Great Dismal Swamp in Virginia.
Photograph of the Great Dismal Swamp in Virginia several years after the 2011 fire. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Photograph of the Great Dismal Swamp in Virginia several years after the 2011 fire. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Cores were collected from various areas of thawing permafrost-peatlands in Alaska. Permafrost thaw results in ground subsidence and inundation that kills black spruce and other understory plants living on the permafrost plateau.
Cores were collected from various areas of thawing permafrost-peatlands in Alaska. Permafrost thaw results in ground subsidence and inundation that kills black spruce and other understory plants living on the permafrost plateau.
Permafrost history in the sporadic zone as context for recent carbon loss using acryostratigraphy, plant macrofossil, and stable isotope approach
Ancient permafrost and past permafrost in the Northern Hemisphere
Practical guide to measuring wetland carbon pools and fluxes
Wetlands cover a small portion of the world, but have disproportionate influence on global carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes. However, the underlying biogeochemical processes that affect wetland C pools and fluxes are complex and dynamic, making measurements of wetland C challenging. Over decades of research, many observational, experimental, and
Past permafrost dynamics can inform future permafrost carbon-climate feedbacks
Panarctic lakes exerted a small positive feedback on early Holocene warming due to deglacial release of methane
Roles of climatic and anthropogenic factors in shaping Holocene vegetation and fire regimes in Great Dismal Swamp, eastern USA
Holocene vegetation dynamics of circum-Arctic permafrost peatlands
Regional variability in peatland burning at mid-to high-latitudes during the Holocene
Permafrost and climate change: Carbon cycle feedbacks from the warming Arctic
Recent climate change has driven divergent hydrological shifts in high-latitude peatlands
Hydrologic controls on peat permafrost and carbon processes: New insights from past and future modeling
Influence of permafrost type and site history on losses of permafrost carbon after thaw
Science and Products
Reconstructing Vegetation and Climate Histories on Palmyra Atoll to Assist with Climate-Smart Adaptation
Holocene and Modern Drivers of Wetland Change
Wetlands in the Quaternary
Wetlands in the Quaternary Project
Charcoal data from four sites in Great Dismal Swamp National Wildlife Refuge - August 2022
Radiocarbon dates, charcoal, and polycyclic aromatic hydrocarbon (PAH) data from Great Dismal Swamp Sites GDS-519 and GDS-520
Carbon budget assessment of tidal freshwater forested wetland and oligohaline marsh ecosystems along the Waccamaw and Savannah rivers, U.S.A. (2005-2016)
Sand Island, one of the first islands on the atoll to have successfully eradicated coconut palms, which were quickly replaced by a healthy Pisonia forest with abundant shorebird life.
Sand Island, one of the first islands on the atoll to have successfully eradicated coconut palms, which were quickly replaced by a healthy Pisonia forest with abundant shorebird life.
A view of the shoreline with palm trees above bright blue water in the Western Lagoon, Palmyra Atoll.
A view of the shoreline with palm trees above bright blue water in the Western Lagoon, Palmyra Atoll.
Aerial view of the Palmyra Atoll, looking west. The forested island is surrounded by blue water.
Aerial view of the Palmyra Atoll, looking west. The forested island is surrounded by blue water.
A recently treated stand of coconut palms, standing and dead, which will naturally convert back to Pisonia forest, on Palmyra Atoll.
A recently treated stand of coconut palms, standing and dead, which will naturally convert back to Pisonia forest, on Palmyra Atoll.
A view of the sandy north shore of Palmyra Atoll, with a forested edge. Recently killed coconut palm trunks poke out of the forested area.
A view of the sandy north shore of Palmyra Atoll, with a forested edge. Recently killed coconut palm trunks poke out of the forested area.
A White Tern and a Red-Footed Booby share some shade under a tree. The White Tern flies while the Booby sits below.
A White Tern and a Red-Footed Booby share some shade under a tree. The White Tern flies while the Booby sits below.
Calm, clear and bright blue waters of a small shoreline lagoon on Palmyra Atoll.
Calm, clear and bright blue waters of a small shoreline lagoon on Palmyra Atoll.
Crystal clear, turquoise waters surrounding a palm-lined beach on Palmyra Atoll.
Crystal clear, turquoise waters surrounding a palm-lined beach on Palmyra Atoll.
Calm, blue waters surround Palmyra Atoll. This view takes in the ocean scenery with a partial glimpse of lush green coastal vegetation on the landward side.
Calm, blue waters surround Palmyra Atoll. This view takes in the ocean scenery with a partial glimpse of lush green coastal vegetation on the landward side.
Driftwood lays partially submerged in clear blue water on sandy shore of Palmyra Atoll.
Driftwood lays partially submerged in clear blue water on sandy shore of Palmyra Atoll.
Photograph of Lake Drummond, which is located within the Great Dismal Swamp in Virginia. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Photograph of Lake Drummond, which is located within the Great Dismal Swamp in Virginia. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Photograph of the Great Dismal Swamp in Virginia.
Photograph of the Great Dismal Swamp in Virginia.
Photograph of the Great Dismal Swamp in Virginia several years after the 2011 fire. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Photograph of the Great Dismal Swamp in Virginia several years after the 2011 fire. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.
Cores were collected from various areas of thawing permafrost-peatlands in Alaska. Permafrost thaw results in ground subsidence and inundation that kills black spruce and other understory plants living on the permafrost plateau.
Cores were collected from various areas of thawing permafrost-peatlands in Alaska. Permafrost thaw results in ground subsidence and inundation that kills black spruce and other understory plants living on the permafrost plateau.
Permafrost history in the sporadic zone as context for recent carbon loss using acryostratigraphy, plant macrofossil, and stable isotope approach
Ancient permafrost and past permafrost in the Northern Hemisphere
Practical guide to measuring wetland carbon pools and fluxes
Wetlands cover a small portion of the world, but have disproportionate influence on global carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes. However, the underlying biogeochemical processes that affect wetland C pools and fluxes are complex and dynamic, making measurements of wetland C challenging. Over decades of research, many observational, experimental, and