Publications
Listed here are publications, reports and articles by the Land Change Science Program in the USGS Ecosystems Mission Area.
Filter Total Items: 1145
Marshes and mangroves as nature-based coastal storm buffers Marshes and mangroves as nature-based coastal storm buffers
Tidal marshes and mangroves are increasingly valued for nature-based mitigation of coastal storm impacts, such as flooding and shoreline erosion hazards, which are growing due to global change. As this review highlights, however, hazard mitigation by tidal wetlands is limited to certain conditions, and not all hazards are equally reduced. Tidal wetlands are effective in attenuating short...
Authors
Stijn Temmerman, Eric Horstman, Ken Krauss, Julia Mullarney, Ignace Pelckmans, Ken Schoutens
The influence of soil development on the depth distribution and structure of soil microbial communities. The influence of soil development on the depth distribution and structure of soil microbial communities.
Although it has been shown that the interaction of climate and time shape the dynamics of soil organic matter (SOM) storage and preservation in soil, the role of soil microbial communities in this dynamic remains unclear. Microbial communities are present throughout soil profiles and likely play critical roles in SOM and nutrient cycling, however the influence of other factors such as...
Authors
Mary-Catherine Leewis, Corey Lawrence, Marjorie S. Schulz, Malak Tfaily, Christian Ayala-Ortiz, Gilberto Flores, Rachel Mackelprang, Jack McFarland
Drought and water management in ancient Maya society Drought and water management in ancient Maya society
Paleoclimate research in the Maya region of Mesoamerica provides compelling evidence of drought during key periods of cultural transition in Maya society. These include the transition from the Preclassic to the Classic, and from Classic to the Postclassic. Previous research emphasized a causal relationship between drought and cultural change, or so-called “collapse” in the Maya region...
Authors
Tripti Bhattacharya, Samantha Krause, Dan Penny, David Wahl
Biostratigraphically significant palynofloras from the Paleocene–Eocene boundary of the USA Biostratigraphically significant palynofloras from the Paleocene–Eocene boundary of the USA
Pollen and spores were recovered from the Paleocene Fort Union Formation and Paleocene–Eocene Willwood Formation of the Bighorn Basin (BHB), northwestern Wyoming, USA. In many local stratigraphic sections in the BHB, the base of the Eocene has been identified by the characteristic negative carbon isotope excursion (CIE) that marks the beginning of the Paleocene–Eocene Thermal Maximum...
Authors
Vera Korasidis, Scott Wing, Guy Harrington, Thomas Demchuk, J. Gfavendyck, Phillip Jardine, Debra A. Willard
Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain
The chronology of the Paleocene-Eocene Thermal Maximum (PETM, ~56 Ma) remains disputed, hampering complete understanding of the possible trigger mechanisms of this event. Here we present an astrochronology for the PETM carbon isotope excursion from Howards Tract, Maryland a paleoshelf environment, on the mid-Atlantic Coastal Plain. Statistical evaluation of variations in calcium content...
Authors
Mingsong Li, Timothy Bralower, Lee Kump, Jean Self-Trail, James Zachos, William Rush, Marci M. Robinson
Assessing reproducibility in sedimentary macroscopic charcoal count data Assessing reproducibility in sedimentary macroscopic charcoal count data
Current understanding of global late Quaternary fire history is largely drawn from sedimentary charcoal data. Since publication, CharAnalysis increasingly has been relied upon as a robust method for analyzing these data. However, several underlying assumptions of the algorithm have not been tested. This study uses replicated charcoal count data to examine the assumption of Poisson...
Authors
Lysanna Anderson, Liubov Presnetsova, David Wahl, Geoffrey Phelps, Alan Gous
The biogeography of relative abundance of soil fungi versus bacteria in surface topsoil The biogeography of relative abundance of soil fungi versus bacteria in surface topsoil
Fungi and bacteria are the two dominant groups of soil microbial communities worldwide. By controlling the turnover of soil organic matter, these organisms directly regulate the exchange of carbon between the soil and the atmosphere. Fundamental differences in the physiology and life history of bacteria and fungi suggest that variation in the biogeography of soil fungal and bacterial...
Authors
Kailiang Yu, Johan Hoogen, Zhiqiang Wang, Colin Averill, Devin Routh, Gabriel Smith, Rebecca Drenovsky, Kate M. Scow, Fei Mo, Mark Waldrop, Yuanhe Yang, Weize Tang, Franciska De Vries, Richard D. Bardgett, Peter Manning, Felipe Bastida, Sara Baer, Elizabeth Bach, Carlos Garcia, Qingkui Wang, Linna Ma, Baodong Chen, Xianjing He, Sven Teurlinex, Amber Heijboer, James Bradley, Thomas Crowther
Floodplain ecology: A novel wetland community of the Amazon Floodplain ecology: A novel wetland community of the Amazon
An expedition to the upper estuarine reaches of the Amazon River reveals intriguing overlap of tropical mangrove wetlands with riverine floodplain forests. This newly discovered type of forested wetland assemblage may provide a uniquely process-rich carbon hotspot.
Authors
Ken Krauss
Quality assurance report for Loch Vale Watershed, 2010–19 Quality assurance report for Loch Vale Watershed, 2010–19
The Loch Vale Watershed Research and Monitoring Program collects long-term datasets of ecological and biogeochemical parameters in Rocky Mountain National Park to support both (1) management of this protected area and (2) research into watershed-scale ecosystem processes as those processes respond to atmospheric deposition and climate variability. The program collects data on...
Authors
Timothy Weinmann, Jill S. Baron, Amanda Jayo
Hydrologic connectivity and residence time affect the sediment trapping efficiency and dissolved oxygen concentrations of the Atchafalaya River Basin Hydrologic connectivity and residence time affect the sediment trapping efficiency and dissolved oxygen concentrations of the Atchafalaya River Basin
Little is known about water movement, volume, or residence time (RT), and how those characteristics affect sediment trapping efficiency (TE) and dissolved oxygen concentrations (DO) in the United States' largest remaining bottomland hardwood swamp, the Atchafalaya River Basin. To better understand these dynamics, this study used bathymetry, lidar, and stage records to determine volumes...
Authors
Daniel Kroes, Richard Day, Michael Kaller, Charles Demas, William Kelso, Tiffany Pasco, Raynie Harlan, Steven Roberts
Simulation of heat flow in a synthetic watershed: Lags and dampening across multiple pathways under a climate-forcing scenario Simulation of heat flow in a synthetic watershed: Lags and dampening across multiple pathways under a climate-forcing scenario
Although there is widespread agreement that future climates tend toward warming, the response of aquatic ecosystems to that warming is not well understood. This work, a continuation of companion research, explores the role of distinct watershed pathways in lagging and dampening climate-change signals. It subjects a synthetic flow and transport model to a 30-year warming signal based on...
Authors
Daniel T. Feinstein, Randall J. Hunt, Eric Morway
Direct and indirect influences of macrophyte cover on abundance and growth of juvenile Atlantic salmon Direct and indirect influences of macrophyte cover on abundance and growth of juvenile Atlantic salmon
1. The relationships between macrophytes and the physical and biological characteristics of the environments that aquatic organisms inhabit are complex. Previous studies have shown that the macrophytes, Ranunculus (subgenus Batrachium), which are dominant in lowland chalk streams and widespread across Europe, can enhance juvenile Atlantic salmon abundance and growth to a greater degree...
Authors
Jessica Marsh, J. Jones, Rasmus Lauridsen, James Grace, Pavel Kratina