Return to Wildland Fire
Return to Northern Bobwhite site
Return to Working Lands for Wildlife site
Return to Working Lands for Wildlife site
Return to SE Firemap
Return to the Landscape Partnership Literature Gateway Website
return
return to main site

Skip to content. | Skip to navigation

Sections

Personal tools

You are here: Home
16 items matching your search terms.
Filter the results.
Item type

























New items since



Sort by relevance · date (newest first) · alphabetically
Project Troff document GTMNERR Community Oyster Shell Recycling and Living Reef Construction Project
This project established an oyster shell recycling program for St. Johns County, Florida, constructed a living shoreline, and planted spartina grass within the boundaries of the new reef to further protect the shoreline and provide nursery habitat for marine species at the Guana Tolomato Matanzas National Estuarine Research Reserve.
Located in Resources / Whitewater to Bluewater W2B
File Integration and scaling of UV-B radiation effects on plants: from DNA to leaf
A process-based model integrating the effects of UV-B radiation through epidermis, cellular DNA, and its consequences to the leaf expansion was developed from key parameters in the published literature. Enhanced UV-B radiation- induced DNA damage significantly delayed cell division, resulting in significant reductions in leaf growth and development. Ambient UV-B radiation-induced DNA damage significantly reduced the leaf growth of species with high relative epidermal absorbance at longer wavelengths and average/low pyrimidine cyclob- utane dimers (CPD) photorepair rates. Leaf expansion was highly dependent on the number of CPD present in the DNA, as a result of UV-B radiation dose, quantitative and qualitative absorptive properties of epidermal pigments, and repair mechanisms. Formation of pyrimidine-pyrimidone (6-4) photoproducts (6-4PP) has no effect on the leaf expansion. Repair mechanisms could not solely prevent the UV-B radiation interference with the cell division. Avoidance or effective shielding by increased or modified qualitative epidermal absorptance was required. Sustained increased UV-B radiation levels are more detri-mental than short, high doses of UV-B radiation. The combination of low temperature and increased UV-B radiation was more significant in the level of UV-B radiation-induced damage than UV-B radiation alone. Slow-growing leaves were more affected by increased UV-B radiation than fast-growing leaves.
Located in Resources / Climate Science Documents
File application/x-internet-signup Medieval warming initiated exceptionally large wildfire outbreaks in the Rocky Mountains
Many of the largest wildfires in US history burned in recent decades, and climate change explains much of the increase in area burned. The frequency of extreme wildfire weather will increase with continued warming, but many uncertainties still exist about future fire regimes, including how the risk of large fires will persist as vegetation changes. Past fire-climate relationships provide an opportunity to constrain the related uncertainties, and reveal widespread burn- ing across large regions of western North America during past warm intervals. Whether such episodes also burned large portions of individual landscapes has been difficult to determine, however, because uncertainties with the ages of past fires and limited spatial resolution often prohibit specific estimates of past area burned. Accounting for these challenges in a subalpine landscape in Colorado, we estimated century-scale fire synchroneity across 12 lake- sediment charcoal records spanning the past 2,000 y. The percent- age of sites burned only deviated from the historic range of vari- ability during the Medieval Climate Anomaly (MCA) between 1,200 and 850 y B.P., when temperatures were similar to recent decades. Between 1,130 and 1,030 y B.P., 83% (median estimate) of our sites burned when temperatures increased ∼0.5 °C relative to the preceding centuries. Lake-based fire rotation during the MCA decreased to an estimated 120 y, representing a 260% higher rate of burning than during the period of dendroecological sampling (360 to −60 y B.P.). Increased burning, however, did not persist throughout the MCA. Burning declined abruptly before temperatures cooled, indicating possible fuel limitations to continued burning.
Located in Resources / Climate Science Documents
Project C source code Restore native aquatic plants in the Santee Cooper system, SC to improve anadromous fish habitat
This project will restore native aquatic plants in the Santee Cooper System (South Carolina) in order to improve anadromous fish habitat.
Located in Resources / Whitewater to Bluewater W2B
Project Stream Bank & Riparian Restoration along the Wild and Scenic Cossatot River on the Ouachita NF
Six riparian sites have severe erosion from loss of riparian vegetation and heavy recreational use. Riparian habitat function will be restored by stabilizing stream banks and planting vegetation. Stream habitat cover will increase with addition of materials to repair stream banks. Campsites will be designated and hardened. To measure effectiveness, water samples taken every 3 months over the past 4 years will continue for at least the next 4 years by the Cossatot River Watch Stream Team to compare pre- and post-restoration.
Located in Resources / Whitewater to Bluewater W2B
File Worldwide evidence of a unimodal relationship between productivity and plant species richness
The search for predictions of species diversity across environmental gradients has challenged ecologists for decades. The humped-back model (HBM) suggests that plant diversity peaks at intermediate productivity; at low productivity few species can tolerate the environmental stresses, and at high productivity a few highly competitive species dominate. Over time the HBM has become increasingly controversial, and recent studies claim to have refuted it. Here, by using data from coordinated surveys conducted throughout grasslands worldwide and comprising a wide range of site productivities, we provide evidence in support of the HBM pattern at both global and regional extents. The relationships described here provide a foundation for further research into the local, landscape, and historical factors that maintain biodiversity.
Located in Resources / Climate Science Documents