Field Survey for Laramie Columbine. (Aquilegia laramiensis) In the Rawlins Field Office

Similar documents
Progress on Defense-Related Uranium Mines Program

Setting the Stage 8/28/09 1. Review. Landscape history of WY. Climate, geology and vegetation patterns in Wyoming

Guidance for implementing the Potential Fossil Yield Classification (PFYC) System

The elevations on the interior plateau generally vary between 300 and 650 meters with

Structural Geology Lab. The Objectives are to gain experience

NOA ASSESSMENT HARRIS QUARRY MENDOCINO COUNTY, CALIFORNIA TABLE OF CONTENTS

Falmouth Town Landing, Falmouth, Maine

Placer Potential Map. Dawson L and U se P lan. Jeffrey Bond. Yukon Geological Survey

ENGINEER S CERTIFICATION OF FAULT AREA DEMONSTRATION (40 CFR )

Amboy Iron Mines, Bristol Mountains, San Bernardino County, California. Gregg Wilkerson 2017

Native species (Forbes and Graminoids) Less than 5% woody plant species. Inclusions of vernal pools. High plant diversity

Prospecting Report 'S Office i DB Property, B.C. -J Negro Creek Nelson Mining District NTS 82F.050. Operator: Kootenay Gold Inc.

!'f \, w. Alan Stewart Colorado Exploration Company, Golden STRUCTURE OF THE FOOTHILLS AREA WEST OF DENVER, COLORADO. Introduction

Hydrogeological Assessment for Part of Lots 2 and 3, Concession 5, Township of Thurlow, County of Hastings 1.0 INTRODUCTION. 1.

TOPOGRAPHIC RELIEF MAP of NYS. LANDFORMS of NYS. Landforms. Creation of NYS Landforms 9/22/2011

A RANGE EXTENSION FOR CYPRIPEDIUM MON- TANUM DOUGLAS EX LINDLEY (ORCHIDACEAE) INTO THE BLACK HILLS OF SOUTH DAKOTA

Colorado Front Range Wildfires Situation Report #7 Monday, July 02, :15 AM (MDT)

THE TOPOGRAPHY AND GEOLOGY OF THE GRAND PORTAGE^

ADDITIONAL PHASE IA ARCHAEOLOGICAL SURVEY FOR THE UMORE PARK SAND AND GRAVEL MINING ENVIRONMENTAL REVIEW SERVICES, DAKOTA COUNTY, MINNESOTA

New Mexico Geological Society

Decoding Topographic Maps

1.8 Ga metamorphic rocks of Mingus Mountain. (Note: All digital images by Prof. C. Merguerian.)

The Little Colorado River

Earth s Layers. Earth s Surface

PALEOGEOGRAPHY of NYS. Definitions GEOLOGIC PROCESSES. Faulting. Folding 9/6/2012. TOPOGRAPHIC RELIEF MAP of NYS GRADATIONAL TECTONIC

The Geology of Sebago Lake State Park

Soils, Hydrogeology, and Aquifer Properties. Philip B. Bedient 2006 Rice University

LANDFORMS of NYS. Landforms. Exercise 4 9/13/2012. TOPOGRAPHIC RELIEF MAP of NYS. Physiographic map of NYS and vicinity showing Surface Features

Observational Data Standard - List of Entities and Attributes

ZONED PEGMATITES OF THE MICANITE DISTRICT FREMONT & PARK COUNTIES, COLORADO

Changes in Texas Ecoregions

Unit 7.2 W.E.D. & Topography Test

MODELING LIGHTNING AS AN IGNITION SOURCE OF RANGELAND WILDFIRE IN SOUTHEASTERN IDAHO

National Wildland Significant Fire Potential Outlook

Last Updated HYDROLOGIC ATLAS OF THE BLACK HILLS, PENNINGTON COUNTY, SOUTH DAKOTA

SOIL INFORMATION FOR PUMPED WATER STORAGE SCHEME, STEELPOORT VALLEY

The subject paper is being submitted for approval for publication in the annual volume entitled Geological Survey Research.

Preliminary Conceptual Model Development

Water, geology, climate & soils: Sierra Nevada, Merced River & Central Valley connections

SCI-5 KES 5.7 Geology Post-test Exam not valid for Paper Pencil Test Sessions

FRACTURE TRACES AND PRODUCTIVITY OF MUNICIPAL WELLS IN THE MADISON LIMESTONE, RAPID CITY, SOUTH DAKOTA

Relative Age-dating -- Discovery of Important Stratigraphic Principles

Spatial Survey of Surface Soil Moisture in a Sub-alpine Watershed Colloquium Presentation, University of Denver, Department of Geography

An Introduction to NatureServe Linking Conservation and Transportation Planning Phoenix, Arizona November 8 & 9, 2006

Detailed Surficial Geologic Mapping and Terrain Analysis of the Blue Hills Felsenmeer Valley, Rusk County, Wisconsin

A Geological Tour of Tumbledown Mountain, Maine

Cape Breton Island Mineral Inventory Studies: A Sandstone Quarry Development Opportunity at Graham River (NTS 11F/14), Inverness County

Geologic Mapping Regional Tournament Trial Event

P.R. SPRING AND HILL CREEK TAR SAND AREAS A RESOURCE ASSESSMENT (IN PROGRESS)

CAUSES FOR CHANGE IN STREAM-CHANNEL MORPHOLOGY

General Editor: Vince Russett

National Wildland Significant Fire Potential Outlook

Relatively little hard substrate occurs naturally in the

=%REPORT RECONNAISSANCE OF CHISHOLM LAKE PROSPECT. October 25, 1977

ENGINEERING EVALUATION OF THE STANLEY MINE ADVENTURE PARK AREA CLEAR CREEK COUNTY, COLORADO. Prepared for:

Hiking the Bold Coast, Cutler, Maine

Why is Sebago Lake so deep?

3.2.2 Ecological units of the Des Quinze lake proposed biodiversity reserve

MIDDLE NORTH PLATTE GLENDO WATERSHED LEVEL 1 STUDY JUNE 2016

Projects and

Data Dictionary for Network of Conservation Areas Transcription Reports from the Colorado Natural Heritage Program

Re: Steep Slope Assessment for 2465 Waverly Drive, Blind Bay, BC; Legal Address: Lot 39, Section 18, Township 22, Range 10, Plan 25579, W6M, KDYD.

An Introduction to Day Two. Linking Conservation and Transportation Planning Lakewood, Colorado August 15-16, 16, 2006

2 Georgia: Its Heritage and Its Promise

Inventory of Plant Species of Special Concern and the General Taxa of Dinosaur National Monument

PRELIMINARY RESULTS AND RECOMMENDATIONS FROM THE NORTHWEST CASCADES TYPE 4/5 STREAM STUDY

Terrain Units PALEOGEOGRAPHY: LANDFORM CREATION. Present Geology of NYS. Detailed Geologic Map of NYS

THE BEDROCK SURFACE AND FORMER DRAINAGE SYSTEMS OF MONTGOMERY COUNTY, OHIO 1

Morphometric Analysis of Chamundi Hills, Mysuru, India Using Geographical Information System

Holocene evolution of Dahab coastline Gulf of Aqaba, Sinai Peninsula, Egypt 1

Structural Geology Lab. The Objectives are to gain experience

Basic Seismological Characterization for Platte County, Wyoming. James C. Case Wyoming State Geological Survey July, 2002 BACKGROUND

PENNSYLVANIA DEPARTMENT OF TRANSPORTATION ENGINEERING DISTRICT 3-0

GLY 155 Introduction to Physical Geology, W. Altermann. Press & Siever, compressive forces. Compressive forces cause folding and faulting.

S6E5: we will investigate the scientific view of how the earth s surface is formed. b. Investigate the contribution of minerals to rock composition

The United States & Canada. A Regional Study of Anglo America

3.1 GEOLOGY AND SOILS Introduction Definition of Resource

Orocopia Sage (Salvia greatae)

Gravel Transport Can Determine Late Flood Tectonics

2. PHYSICAL SETTING FINAL GROUNDWATER MANAGEMENT PLAN. 2.1 Topography. 2.2 Climate

GET TO KNO W A NATIO NAL

Describing Greater sage-grouse (Centrocercus urophasianus) Nesting Habitat at Multiple Spatial Scales in Southeastern Oregon

Weather and Climate of the Rogue Valley By Gregory V. Jones, Ph.D., Southern Oregon University

EVALUATION OF SLOPE STABILITY NEAR LOTS #3-6, LOWER ICEHOUSE CANYON ROAD, MT. BALDY, CALIFORNIA

COOMALIE RIDGES RADIOMETRIC SURVEY, RUM JUNGLE AREA,

Chitra Sood, R.M. Bhagat and Vaibhav Kalia Centre for Geo-informatics Research and Training, CSK HPKV, Palampur , HP, India

APPENDIX E. GEOMORPHOLOGICAL MONTORING REPORT Prepared by Steve Vrooman, Keystone Restoration Ecology September 2013

Ecoregions Glossary. 7.8B: Changes To Texas Land Earth and Space

Data Dictionary for Potential Conservation Area Transcription Reports from the Colorado Natural Heritage Program

Survey & Manage Compliance Report Pettijohn LSR Project Tom Quinn April 13, 2011 Updated and Edited by Kelly Wolcott May 4, 2011.

Sacred Lands File & Native American Contacts List Request

TESTING FUNCTIONAL RESTORATION OF LINEAR FEATURES PHASE I PROGRESS REPORT WITHIN BOREAL CARIBOU RANGE

Photo 119. Ripple marks in the Gordon Lake Formation. Highway 639 at the entrance to Laurentian Lodge.

Pine Hill Serpentinized Peridotite,

ANALYSIS OF GLACIER CHANGE IN THE SIERRA NEVADA PORTLAND STATE UNIVERSITY DEPARTMENT OF GEOLOGY BRADLEY BUSELLI

depression above scarp scarp

Cenozoic Extensional Basin Development and Sedimentation in SW Montana

LANDSAT-TM IMAGES IN GEOLOGICAL MAPPING OF SURNAYA GAD AREA, DADELDHURA DISTRICT WEST NEPAL

Report: rock sample collection in the Northern Cape

FIRST YEAR ASSESSMENT REPORT PROSPECTING LICENCE 16512M MARYSTOWN AREA, BURIN PENINSULA NTS 1M/3

Transcription:

Field Survey for Laramie Columbine (Aquilegia laramiensis) In the Rawlins Field Office prepared for the Wyoming Natural Diversity Database, University of Wyoming, and the Bureau of Land Management, Rawlins Field Office by Hollis Marriott and Dennis Horning Laramie, Wyoming November 1, 2004

Acknowledgements We thank botanist Bonnie Heidel and data manager/gis master Tessa Dutcher of the Wyoming Natural Diversity Database, University of Wyoming, for overseeing the survey project, and providing GIS data and maps. Frank Blomquist of the Rawlins Field Office (BLM) quickly obtained the permission we needed to cross private land to survey sites of interest. We are grateful to the landowners that allowed access across their lands, and that shared with us their knowledge and appreciation of the area. Thanks once again to the staff of the Rocky Mountain Herbarium, University of Wyoming, for continued use of their fine facility. Report Citation Marriott, H. and D. Horning. 2004. Field survey for Laramie columbine (Aquilegia laramiensis) in the Rawlins Field Office. Unpublished report prepared for the Wyoming Natural Diversity Database, University of Wyoming, and the Bureau of Land Management, Rawlins Field Office.

Introduction The Laramie columbine, Aquilegia laramiensis, is restricted to the Laramie Mountains in southeast Wyoming (Figure 1). It is listed as a Sensitive species by the Forest Service and Bureau of Land Management, and is ranked G2S2 by the Wyoming Natural Diversity Database (WYNDD), defined as imperiled because of rarity on a global and state basis (Keinath et al. 2003). The species was first collected in 1895 by Aven Nelson at the foot of Laramie Peak in the northern Laramie Mountains. He published a description of the species the next year (Nelson 1896). Nelson made more collections in 1900 and 1901, extending the known range to Ragged Top Mountain east-northeast of Laramie. The next new records for the columbine were not reported until the 1970s and 1980s. All were in the northern Laramie Mountains in the general area of Laramie Peak. In 1993, C. Refsdal collected the columbine roughly halfway between Laramie Peak and Ragged Top Mountain. Several new records were found during general floristic surveys of the area (Packer 2000), including a range extension about 16 miles to the northwest in the vicinity of School Section Mountain by B.E. Nelson in 1997. By 2002, the species was known from 13 sites; two of these are considered historical without precise location data. Systematic survey for the Laramie columbine began in 2003, on Forest Service lands in the northern Laramie Mountains (Marriott and Horning 2004). Twenty new sites were found, but the overall distribution remained limited, with most populations clustered in the northern part of the range. Survey was recommended for Bureau of Land Management (BLM) lands in the northern Laramie Range, based on the existence of known potential habitat for the species. In 2004, we entered into an agreement with the Wyoming Natural Diversity Database (WYNDD) to conduct surveys for Aquilegia laramiensis on lands managed by the Rawlins Field Office, with funding provided by the BLM. Study Area The Laramie Mountains, in southeast Wyoming, extend north and then northwest from northeast Colorado near the Wyoming border approximately 140 miles, ending in the vicinity of Douglas, Wyoming. The range is typical of the Laramide mountain-building episode, when most of the Rocky Mountain ranges were uplifted. It is a broad anticline with sedimentary rocks exposed on the flanks. Precambrian intrusive and metamorphic rocks are found at high elevations (Blackstone 1996). Geology of the study area is described in detail in our previous report (Marriott and Horning 2004). Many of the 2004 survey sites are within an area that has been called the Central Metamorphic Complex (Johnson and Hills 1976). Bedrock includes Archean (earlier Precambrian) metamorphic rocks, mainly gneiss. This is in contrast with the 2003 study area to the north, which is underlain by Archean

granite. The 2004 study area is lower in elevation, drier and has less tree cover compared to sites surveyed in 2003. Because Aquilegia laramiensis is associated with cooler, more mesic sites, there was less potential habitat to be surveyed. Figure 1. Range of Aquilegia laramiensis (map by WYNDD).

Methods Our primary goal was to document distribution and abundance of Aquilegia laramiensis on BLM lands. This basic information is required to determine whether Sensitive status is warranted for the species. If rangewide survey shows that special management is warranted, additional information should be collected for a better understanding of the species and its needs. Survey Site Selection Because there had been little survey for the columbine in the study area, we covered as many sites as possible well-distributed through the area to determine the range and rarity of the species. Field work was restricted to lands managed by the BLM, Rawlins Field Office, for the most part. Some State land was visited when in proximity. Private land was crossed occasionally with permission, but no surveys for Laramie columbine were made on private lands. Maps of survey sites are on file at WYNDD. Aquilegia laramiensis usually is found on well-shaded sites with little vegetative cover. Our surveys in 2003 showed that large granite outcrops with steep northerly aspects were most likely to support columbine populations, and these were highest priority for survey in 2004. Less prominent outcrops were checked when easily accessed. Suitable outcrops were identified on topographic maps rather than aerial photos, which do not show vertical relief as well. Horning s familiarity with the area, specifically locations of large rock outcrops and access routes, was quite helpful. Data Collection Survey began on June 11 and continued through early July. Because the primary goal of this project was to visit as many potential sites as possible, data collection was kept simple. Generally, less than one hour was spent at a site, with access much more time-consuming. No effort was made to find every plant at a site; some populations may be significantly larger than documented. Data collection was designed to accurately document locations, estimate population size, characterize habitat qualitatively, note any obvious threats or potential threats, and identify any unsurveyed potential habitat in the area. A sample survey form is included in Appendix A at the end of this report. Photographs of plants and habitat are on file at WYNDD. All populations were sufficiently large to allow collection of voucher material. Specimens are deposited at the Rocky Mountain Herbarium (RM) at the University of Wyoming in Laramie.

Results Twelve new occurrences of Aquilegia laramiensis were found in 2004, bringing the total known to 45. Two of these are historical records without precise location information. The known range of the species was expanded, mainly to the southeast, but its overall range remains limited (Figure 2). Most Laramie columbine populations are small. Population size correlates with outcrop size and microsite availability, as was observed in 2004. Where there are extensive systems of rock outcrops with appropriate microsites, the Laramie columbine occurs as many patches. At such sites, several hundred above-ground individuals were estimated within areas surveyed, with total populations probably larger. Some of the outcrops where the columbine was found in 2004 are small and at lower elevations compared with 2003 survey sites. In these situations populations are quite small (20-30 plants). Additional information on habitat was collected in 2004. The elevational range of Aquilegia laramiensis was extended down to 5400 ft (previously the lowest known site was at 6250 ft). As was seen in 2003, the species grows on most aspects, rather than just northerly as originally reported. All microsites were well shaded in some fashion. The columbine was found on several types of igneous and metamorphic rock, including granite, gneiss and peridotite. As was observed in 2003, it is absent from a reddish coarse-grained granite found in parts of the study area (see Marriott and Horning 2004 for additional information on rock types and habitat suitability). After the 2003 field season, we reported that the rugged habitat of Aquilegia laramiensis is largely inaccessible, and that no significant threats to overall viability are apparent (Marriott and Horning 2004). Some sites surveyed in 2004 are more easily reached, including several with very small populations. Conservation needs are discussed below under Conservation Status. Discussion Additional Survey Needs Surveys 2003 and 2004 significantly increased the information available regarding distribution and status of Aquilegia laramiensis. However there remain large areas of unsurveyed potential habitat, mainly large complex systems of rock outcrops on Medicine Bow National Forest in the northern Laramie Mountains. Most of these sites are difficult to access, and survey will take significantly more time compared with work done in 2003 and 2004. There is additional unsurveyed potential habitat on BLM lands west and north of Medicine Bow National Forest. These are managed by the Casper Field Office, and were not included in the 2004 field project. Some sites are thought to have high potential for Laramie columbine, including lands immediately

adjacent to the northwest part of Medicine Bow National Forest where the species was documented in 2003 (Deer Creek). Figure 2. Range of Aquilegia laramiensis in southeast Wyoming, showing new sites found during the 2004 field season (map by WYNDD).

Conservation Status The Laramie columbine is now known from 43 sites, with two additional reports that are considered historical without precise location information. Most of the sites are in the northern Laramie Mountains, within an area approximately 35 air miles in length, with a few disjunct populations as far south as Ragged Top Mountain east-northeast of Laramie. The overall range of the species remains limited, and populations are small. There are no obvious threats to overall viability of the Laramie columbine at this time. The rugged terrain of many sites makes access difficult. At more accessible locations, collecting for cultivation may be a concern, but has not been documented at this time. However, it is known that the species is of interest to gardeners (e.g. Nold 2003). Several sites documented in 2004 were on small outcrops at lower elevations. In these situations, populations are quite small, and collecting could significantly impact or extirpate the species. Grazing, timber harvest and recreation do not pose obvious threats currently. Columbine populations appear to tolerate fire, mainly because there is little fuel on rock outcrops where the plants grow; shading is provided by aspect and topography rather than trees in most cases. A more thorough discussion of possible impacts and conservation needs is included in our earlier report, and remains relevant (Marriott and Horning 2004). Literature Cited Blackstone, D. L., Jr. 1996. Structural geology of the Laramie Mountains, southeastern Wyoming and northeastern Colorado. Rep. of Investigations No. 51. WY State Geol. Survey, Laramie. Johnson, R.C. and F.A. Hills. 1976. Precambrian geochronology and geology of the Boxelder Canyon area, northern Laramie Range, Wyoming. Geol. Soc. of America Bull. 87: 809-817. Keinath, D., B. Heidel and G. Beauvais. 2003. Wyoming plant and animal species of concern. Laramie, WY: Wyoming Natural Diversity Database, Univ. WY. Marriott, H. and D. Horning. 2004. Status of Laramie columbine (Aquilegia laramiensis) and results of field survey. Unpublished report prepared for the Wyoming Natural Diversity Database, University of Wyoming, and Medicine Bow National Forest, Laramie, WY. Nelson, A. 1896. First report on the flora of Wyoming. WY Agr. Exp. Sta. Bull. 28:78-79. Nold, R. 2003. Columbines: Cambridge: Timber Press.

Appendix A. Field form used in 2004 surveys for Aquilegia laramiensis.

Appendix B. Aquilegia laramiensis element occurrences and maps.