scholarly journals Holocene geo-ecological evolution of Lower Geyser Basin, Yellowstone National Park (USA)

2021 ◽  
pp. 1-17
Author(s):  
Christopher M. Schiller ◽  
Cathy Whitlock ◽  
Sabrina R. Brown
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Forest Cover ◽  
Vegetation History ◽  
Fire Regime ◽  
Water Discharge ◽  
Hydrothermal Activity ◽  
Sediment Geochemistry ◽  
Thermal Waters ◽  
History Of

Abstract Changes in climate and fire regime have long been recognized as drivers of the postglacial vegetation history of Yellowstone National Park, but the effects of locally dramatic hydrothermal activity are poorly known. Multi-proxy records from Goose Lake have been used to describe the history of Lower Geyser Basin where modern hydrothermal activity is widespread. From 10,300 cal yr BP to 3800 cal yr BP, thermal waters discharged into the lake, as evidenced by the deposition of arsenic-rich sediment, fluorite mud, and relatively high δ13Csediment values. Partially thermal conditions affected the limnobiotic composition, but prevailing climate, fire regime, and rhyolitic substrate maintained Pinus contorta forest in the basin, as found throughout the region. At 3800 cal yr BP, thermal water discharge into Goose Lake ceased, as evidenced by a shift in sediment geochemistry and limnobiota. Pollen and charcoal data indicate concurrent grassland development with limited fuel biomass and less fire activity, despite late Holocene climate conditions that were conducive to expanded forest cover. The shift in hydrothermal activity at Goose Lake and establishment of the treeless geyser basin may have been the result of a tectonic event or change in hydroclimate. This record illustrates the complex interactions of geology and climate that govern the development of an active hydrothermal geo-ecosystem.

scholarly journals Fire History of the Lamar River Drainage, Yellowstone National Park, Wyoming

1989 ◽  
Vol 13 ◽  
pp. 169-173
Author(s):  
Stephen Barrett ◽  
Stephen Arno
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Fire History ◽  
Fire Regime ◽  
Lodgepole Pine ◽  
Fire Regimes ◽  
Pine Forests ◽  
River Drainage ◽  
Tree Ring Data ◽  
History Of

This study's goal is to document the fire history of the Lamar River drainage, southeast of Soda Butte Creek in the Absaroka Mountains of northeastern Yellowstone National Park (YNP). Elsewhere in YNP investigators have documented very long-interval fire regimes for lodgepole pine forests occurring on rhyolitic derived soils (Romme 1982, Romme and Despain 1989) and short-interval fire regimes for the Douglas-fir/grassland types (Houston 1973). No fire regime information was available for lodgepole pine forests on andesitic derived soils, such as in the Lamar drainage. This study will provide managers with a more complete understanding of YNP natural fire history, and the data will supplement the park's Geographic Information System (GIS) data base. Moreover, most of the study area was severely burned in 1988 and historical tree ring data soon will be lost to attrition of potential sample trees.

scholarly journals Atlas of Yellowstone, 2nd Edition: Celebrating 150 Years of the World’s First National Park, 1872–2022

2019 ◽  
Vol 1 ◽  
pp. 1-1
Author(s):  
W. Andrew Marcus ◽  
James E. Meacham ◽  
Justin T. Menke ◽  
Aleathea Y. Steingisser ◽  
Ann E. Rodman
Keyword(s):  
Key Management ◽  
Yellowstone National Park ◽  
National Park ◽  
Scientific Data ◽  
Light Pollution ◽  
Natural Setting ◽  
The World ◽  
History Of ◽  
The Many ◽  
Management Issues

<p><strong>Abstract.</strong> The Second Edition of the Atlas of Yellowstone will celebrate the 150-year history of the world’s first national park – and reflect on the future of Yellowstone and its evolving place in the world. Like the first Atlas of Yellowstone published in 2012, the Second Edition will provide a comprehensive view of the human and natural setting of Yellowstone National Park. Also like the First Edition, the new edition will portray variations over space and time, explore human-nature interactions throughout the region, document connections of Yellowstone to the rest of the world, and &amp;ndash; ultimately &amp;ndash; guide the reader to a deeper appreciation of Yellowstone.</p><p>Beyond that, the new edition will provide much expanded coverage of the park’s history. Readers will better understand the many different ways in which the creation of Yellowstone National Park has preserved and altered the landscapes and ecology of Yellowstone and conservation thought and practice, both locally and around the world.</p><p>The new atlas will also reflect advances in scientific data collection, knowledge, and insight gained since publication of the first edition. New topic pages will address key management issues ranging from increased visitor impact to wildlife disease to light pollution. In addition, many of the 850 existing graphics will be updated, reimagined, or replaced by new graphics that capture the remarkable wealth of data that has become available since the First Edition. Whether it be tracking of individual wolves, ecosystem imagery from space, or detailed visitor surveys &amp;ndash; new data provide insights that could not be graphically displayed before.</p><p>The Second Edition celebrates 150 years of America’s best idea and what that has meant to the world. The significance of Yellowstone National Park to conservation, scholarship, and the human experience is enormous, and deserves a volume that captures that importance.</p>

scholarly journals A Comparison of Fire Regimes and Stand Dynamics in Whitebark Pine (Pinus albicaulis) Communities in the Greater Yellowstone Ecosystem

2003 ◽  
Vol 27 ◽  
pp. 123-128
Author(s):  
William Romme ◽  
James Walsh
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Fire Regime ◽  
Fire Regimes ◽  
Greater Yellowstone Ecosystem ◽  
Past Century ◽  
Grizzly Bear ◽  
Pinus Albicaulis ◽  
Whitebark Pine ◽  
Greater Yellowstone

Whitebark pine (Pinus albicaulis) is a keystone species of upper subalpine ecosystems (Tomback et al. 2001), and is especially important in the high-elevation ecosystems of the northern Rocky Mountains (Arno and Hoff 1989). Its seeds are an essential food source for the endangered grizzly bear (Ursus arctos horribilis), particularly in the autumn, prior to winter denning (Mattson and Jonkel 1990, Mattson and Reinhart 1990, Mattson et al. 1992). In the Greater Yellowstone Ecosystem (GYE), biologists have concluded that the fate of grizzlies is intrinsically linked to the health of the whitebark pine communities found in and around Yellowstone National Park (YNP) (Mattson and Merrill 2002). Over the past century, however, whitebark pine has severely declined throughout much of its range as a result of an introduced fungus, white pine blister rust (Cronartium ribicola) (Hoff and Hagle 1990, Smith and Hoffman 2000, McDonald and Hoff 2001), native pine beetle (Dendroctonus ponderosae) infestations (Bartos and Gibson 1990, Kendall and Keane 2001), and, perhaps in some locations, successional replacement related to fire exclusion and fire suppression (Amo 2001). The most common historical whitebark pine ftre regimes are "stand-replacement", and "mixed­ severity" regimes (Morgan et al. 1994, Arno 2000, Arno and Allison-Bunnell2002). In the GYE, mixed-severity ftre regimes have been documented in whitebark pine forests in the Shoshone National forest NW of Cody, WY (Morgan and Bunting 1990), and in NE Yellowstone National Park (Barrett 1994). In Western Montana and Idaho, mixed fire regimes have been documented in whitebark pine communities in the Bob Marshall Wilderness (Keane et al. 1994), Selway-Bitterroot Wilderness (Brown et al. 1994), and the West Bighole Range (Murray et al.1998). Mattson and Reinhart (1990) found a stand­replacing fire regime on the Mount Washburn Massif, within Yellowstone National Park.

Selling Yellowstone: Capitalism and the Construction of Nature. By Mark Daniel Barringer. Lawrence: University Press of Kansas, 2002. Pp. viii, 238. $29.95.

2003 ◽  
Vol 63 (1) ◽  
pp. 276-277
Author(s):  
Robert K. Fleck
Keyword(s):  
Interest Groups ◽  
Yellowstone National Park ◽  
National Park ◽  
Public Lands ◽  
Detailed History ◽  
Private Provision ◽  
Goods And Services ◽  
History Of

In this well written book, Mark Barringer provides an interesting and detailed history of commercial enterprises in Yellowstone National Park. The book has great value to scholars concerned with the management of public lands, the roles that interest groups (park employees, concessioners, tourists, and environmentalists) have played in the history of Yellowstone, and the difficulties in designing contracts for the private provision of goods and services on public lands.

Fluoride geochemistry of thermal waters in Yellowstone National Park: I. Aqueous fluoride speciation

2011 ◽  
Vol 75 (16) ◽  
pp. 4476-4489 ◽  
Author(s):  
Yamin Deng ◽  
D. Kirk Nordstrom ◽  
R. Blaine McCleskey
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Thermal Waters

Ammonium in thermal waters of Yellowstone National Park: Processes affecting speciation and isotope fractionation

2011 ◽  
Vol 75 (16) ◽  
pp. 4611-4636 ◽  
Author(s):  
JoAnn M. Holloway ◽  
D. Kirk Nordstrom ◽  
J.K. Böhlke ◽  
R. Blaine McCleskey ◽  
James W. Ball
Keyword(s):  
Yellowstone National Park ◽  
National Park ◽  
Isotope Fractionation ◽  
Thermal Waters

scholarly journals Late-Glacial and Postglacial Vegetation and Climate of Jackson Hole and the Pinyon Peak Highlands, Wyoming

1985 ◽  
Vol 9 ◽  
pp. 44-49
Author(s):  
Cathy Barnosky
Keyword(s):  
Rocky Mountains ◽  
National Park ◽  
Vegetation History ◽  
Late Quaternary ◽  
Late Glacial ◽  
Glacial Refugia ◽  
Northern Rocky Mountains ◽  
Jackson Hole ◽  
History Of ◽  
Vegetation And Climate

The late-Quaternary vegetation history of the northern Rocky Mountains has thus far been inferred largely from isolated records. These data suggest that conifer forests were established early in postglacial time and were little modified thereafter. The similarity of early postglacial vegetation to modern communities over broad areas gives rise to two hypotheses: (1) that glacial refugia were close to the ice margin, and (2) that vegetation soon colonized the deglaciated areas and has been only subtly affected by climatic perturbations since that time. It is the goal of this project to test these two hypotheses in the region of Grand Teton National Park.

scholarly journals Recent Debris-Flow and Flash-Flood History of Northeastern Yellowstone National Park

1996 ◽  
Vol 20 ◽  
pp. 3-11
Author(s):  
Joshua Landis ◽  
Grant Meyer
Keyword(s):  
Debris Flow ◽  
Yellowstone National Park ◽  
Little Ice Age ◽  
National Park ◽  
Flash Flood ◽  
Global Climate ◽  
Ice Age ◽  
Drought Severity ◽  
History Of ◽  
Flow Activity

An understanding of the ecological health of stream systems and riparian areas in Yellowstone National Park (YNP) requires knowledge of their response to climatic and hydrological influences; intrinsic factors such as relief and geological materials are important influences as well (e.g., O'Hara and Meyer 1995). Recent studies of southwestern (Ely et al. 1993) and midwestern U.S. rivers (Knox 1993) have shown that relatively minor climatic changes in the late Holocene are associated with large fluctuations in flood magnitude and frequency. In small, steep drainage basins of northeastern YNP (Figure 1), Meyer et al. (1992, 1995) associated increased fire-related debris-flow activity with decadal to millennial-scale cycles of drought over the Holocene. Observations of modern events indicate that debris-flow and flash floods are also produced in the absence of fire in this rugged mountainous region, primarily by intense summer thunderstorm precipitation. Although a correlation between drought severity and fire magnitude in Yellowstone is clear (Balling et al. 1992a, 1992b), the relationship hypothesized by Meyer et al. (1992,1995) between warm, drought-prone climatic episodes and debris-flow activity in this region requires further investigation. Therefore, we use relatively high-resolution lichenometric and tree­ring dating methods to construct a 250-year history of major hydrologic events in small, steep tributary basins of Soda Butte Creek in northeastern Yellowstone. This period spans the transition from the generally cooler global climate of the Little Ice Age to the present (e.g., Grove 1988). Although the Little Ice Age was not uniformly cold in either a spatial or temporal sense (Jones and Bradley 1995), and YNP climate is not well known in the earlier part of this interval, trends toward increasing summer temperatures and decreasing winter precipitation in YNP over the last ~100 yr are consistent with this transition (Balling et al. 1992a).

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