The conference was fortunate to have two knowledgeable and experienced speakers for the week! Husband-and-wife-team Chris Swarth and Marilyn Fogel each had tremendous information and insight to share, along with a special family research project. Check out their introductory presentation.
Saturday
SINHC 2012 Speakers
The conference was fortunate to have two knowledgeable and experienced speakers for the week! Husband-and-wife-team Chris Swarth and Marilyn Fogel each had tremendous information and insight to share, along with a special family research project. Check out their introductory presentation.
Chris Swarth
Chris Swarth, Natural History Conference speaker for the week, is a naturalist and director of the Jug Bay Wetlands Sanctuary in Maryland, a freshwater tidal wetlands on the coast. Chris notes that there are many species of plants and animals at Jug Bay. A few details: Wild rice is important plant there for lots of different species—a native plant, many creatures depend upon it. There’s a nature center where they stage programs and exhibits; they train lots of volunteers to work with them on "citizen science." They use fences to enclose small areas in an effort to protect the wild rice from the geese. Jug Bay has had a banding station in operation for about 20 years, studying local songbirds such as cardinals or wood thrush. In addition to their work with birds, they attach transmitters to turtles to gather information about them.
Marilyn Fogel

Marilyn L. Fogel, Senior Staff Scientist, Carnegie Institution for Science Geophysical Laboratory, is Chris' wife and co-speaker for the conference. She is a biogeochemist or geobiologist; Marilyn studies the modern environment to learn about the past. She has work with mangrove ecosystems in the tropics, Belize, studying how they respond to different nutrient conditions; she and her colleagues also work in the lab. Some of her work involves growing microbes in extreme conditions, revealing how life is not just on the surface but extends deep into the oceans and into rocks. She notes that stable isotopes have been around for 8-9 billion years. “You think you’re old—those isotopes are older; they ended up on the planet, and they ended up in you.”
Low-Tide Walk
Exploring the Coast of Maine
Cassie Durette, program coordinator for the Northeastern Regional Association of Coastal and Ocean Observing Systems of (NERACOOS), talked about data collection in the Isles of Shoals. She noted that there has been a significant increase in ocean acidification in our lifetime. Impacts on phytoplankton are very important because its health is key to ocean ecosystems. A buoy off the coast of Appledore Island measures ocean acidification/Co2. Appledore is an AirMap station. Ways they observe: drifters; satellites; gliders. There are a variety of buoy types. Buoys collect information on: Co2 atmospheric pressure, chlorophyll, nutrients, currents, dissolved oxygen, visibility, water temperature, wind, waves, and air temperature. The information (data) is collected by different sensors.
Seabirds: Their Lives and Ecology
Presentation
Another adaptation: their eggs have a shape that’s unlikely to roll off--it is very tapered on one end. Each egg has a characteristic color and pattern to help pairs recognize their eggs in crowded breeding colonies.
Dynamic soaring: Birds can soar or fly without flapping their wings. Soaring birds go in an up-and-down pattern: climb, change of flight direction to leeward, descent (leeward), climb (windward).
Convergent Evolution: Penguins and Auks exhibit convergent evolution. Though adaptation to similar ecosystems and life styles these unrelated bird families have evolved similar body plans.
Common seabirds of the Gulf of Maine
• Cormorants
• Storm-Petrels
• Shearwaters
• Diving ducks (eider) Gulls and terns (laughing hgull, herring, black backed, common tern, arctic tern, roseate tern, least tern
• Alcids
Although many fisheries are depleted, there is still a rich ecosystem to support these birds.
The currents bring the nutrients into the area; the winds that move across the ocean, that power the flights of the birds from the south are also important. Birds can read the winds and the currents and find the food.
Seabirds are linked to the ocean environment; the only time they are not on the ocean is when they are nesting. Examples: albatrosses, petrels, boobies, auks frigatebirds, penguins, phalaropes, long tailed ducks, sabine’s gull, arctic tern, black-legged kittwoke.
Characteristics:
• Long-lived (20-60 years)
• Delayed sexual maturity: up to 10 years
• Small clutch size: often just 1 egg
• High degree of parental care
• Long fledgling period
• Usually monogamous; some mate for life
• 95% of species nest in colonies, some with 1000s of pairs
• Often nest on islands or cliffs safe from mammalian predators
• High degree of breeding site fidelity and philopatry
• Special adaptations to a marine life
Seabird adaptations
• Dense plumage
• Superior waterproofing
• Countershading plumage: dark above, light below
• Strong, flexible webbed feet
Characteristics:
• Long-lived (20-60 years)
• Delayed sexual maturity: up to 10 years
• Small clutch size: often just 1 egg
• High degree of parental care
• Long fledgling period
• Usually monogamous; some mate for life
• 95% of species nest in colonies, some with 1000s of pairs
• Often nest on islands or cliffs safe from mammalian predators
• High degree of breeding site fidelity and philopatry
• Special adaptations to a marine life
Seabird adaptations
• Dense plumage
• Superior waterproofing
• Countershading plumage: dark above, light below
• Strong, flexible webbed feet
Another adaptation: their eggs have a shape that’s unlikely to roll off--it is very tapered on one end. Each egg has a characteristic color and pattern to help pairs recognize their eggs in crowded breeding colonies.
Dynamic soaring: Birds can soar or fly without flapping their wings. Soaring birds go in an up-and-down pattern: climb, change of flight direction to leeward, descent (leeward), climb (windward).
Convergent Evolution: Penguins and Auks exhibit convergent evolution. Though adaptation to similar ecosystems and life styles these unrelated bird families have evolved similar body plans.
Common seabirds of the Gulf of Maine
• Cormorants
• Storm-Petrels
• Shearwaters
• Diving ducks (eider) Gulls and terns (laughing hgull, herring, black backed, common tern, arctic tern, roseate tern, least tern
• Alcids
Although many fisheries are depleted, there is still a rich ecosystem to support these birds.
The currents bring the nutrients into the area; the winds that move across the ocean, that power the flights of the birds from the south are also important. Birds can read the winds and the currents and find the food.
Oceans, People & Changing Climate
Marilyn connected her work analyzing isotopes to climate change.

o Carbon Dioxide: CO2
o Methane: CH4
o Water Vapor: H2O
o Nitrous Oxide: N2O
If you go out and measure the isotopes, you can tell that the isotopes have changed; it is possible to ascertain that they came from fossil fuel.
• The currents and land masses that we have are the ones we’ve evolved with; they were not "always" this way! If the patterns change, it has significant implications for the Earth.
Discussion:
• Great Ocean Conveyor Belt that moves nutrients around the world is density-driven: Salty, cold water is heavy
• Heat bounces back down from layer of greenhouse gases (trivia: The major source of pollution in Los Angeles basin=cows)
What’s the difference between climate and weather? Arguments one has on airplanes.
o Weather: It rained today
o Climate: Averages, statistics
• What happens as the Earth’s temperature increases?
o Ice melts, sea level rises=flooding, gyres change
o As you start to heat the land and air, the wind direction changes
o Will the conveyor belt stop? No-one really knows.
Conclusion:
• The heat content of the ocean has increased from 1960 to the present: 1.15 c
• Ocean circulation may change, and may even shut down
• Oceans will absorb CO2, and change the chemistry enough to affect organisms
• Sea level has risen due to melting ice caps and sea ice: about 60mm
ce caps and sea ice: about 60mm
Presentation
Heavy and Light Stable Isotopes—Lighter isotopes react/move faster than heavy isotopes (Just like some people). Greenhouse gas consists of:
Heavy and Light Stable Isotopes—Lighter isotopes react/move faster than heavy isotopes (Just like some people). Greenhouse gas consists of:
o Carbon Dioxide: CO2
o Methane: CH4
o Water Vapor: H2O
o Nitrous Oxide: N2O
If you go out and measure the isotopes, you can tell that the isotopes have changed; it is possible to ascertain that they came from fossil fuel.
• The currents and land masses that we have are the ones we’ve evolved with; they were not "always" this way! If the patterns change, it has significant implications for the Earth.
Discussion:
• Great Ocean Conveyor Belt that moves nutrients around the world is density-driven: Salty, cold water is heavy
• Heat bounces back down from layer of greenhouse gases (trivia: The major source of pollution in Los Angeles basin=cows)
What’s the difference between climate and weather? Arguments one has on airplanes.
o Weather: It rained today
o Climate: Averages, statistics
• What happens as the Earth’s temperature increases?
o Ice melts, sea level rises=flooding, gyres change
o As you start to heat the land and air, the wind direction changes
o Will the conveyor belt stop? No-one really knows.
Conclusion:
• The heat content of the ocean has increased from 1960 to the present: 1.15 c
• Ocean circulation may change, and may even shut down
• Oceans will absorb CO2, and change the chemistry enough to affect organisms
• Sea level has risen due to melting ice caps and sea ice: about 60mm
ce caps and sea ice: about 60mm
Seabirds, Part II
One thing that keeps birds more waterproof—especially sea birds—is the preen or uropygial gland, which produces oil that is distributed to feathers while preening. Seabirds and diving ducks have extra-large ones of these. The Herring Gull breeds all across Canada, and they breed inland. Not all gulls are over the sea, so “seagulls” is a misnomer.
Types of gull (note: not all are "seagulls!")
The Great Black-backed Gull: There are many of these in the Isles of Shoals. It takes these largest of the gulls four years to grow to full maturity. Because they need a lot of experience to be successful breeders they must be in full adult plumage (which signals maturity) before they can breed. The Herring and Great Black-backed are pink-legged gulls. Waterbirds have a countercurrent to cool extremities, which minimizes heat loss to the cold environment. Heat flows from arteries to veins along the length of the leg. This conserves body heat.
Laughing Gull: Have a very distinctive, deeper call than the Herring Gull. It’s part of a group of gulls that get a distinctive plumage change with a hood during the breeding season. These are comparatively small.
The Ring-billed Gull is a smaller, not-pink-legged gull that takes 3 years to get adult plumage.
Bonaparte’s Gull is a pelagic bird that will get quite far out in the ocean.
Black-legged Kitiwake: A very pelagic gull, seldom near land. Very delicate. There are several species of Kitiwake. They nest on tiny ledges on vertical cliffs in Norway or Alaska.
The Great Black-backed Gull: There are many of these in the Isles of Shoals. It takes these largest of the gulls four years to grow to full maturity. Because they need a lot of experience to be successful breeders they must be in full adult plumage (which signals maturity) before they can breed. The Herring and Great Black-backed are pink-legged gulls. Waterbirds have a countercurrent to cool extremities, which minimizes heat loss to the cold environment. Heat flows from arteries to veins along the length of the leg. This conserves body heat.
Laughing Gull: Have a very distinctive, deeper call than the Herring Gull. It’s part of a group of gulls that get a distinctive plumage change with a hood during the breeding season. These are comparatively small.
The Ring-billed Gull is a smaller, not-pink-legged gull that takes 3 years to get adult plumage.
Bonaparte’s Gull is a pelagic bird that will get quite far out in the ocean.
Black-legged Kitiwake: A very pelagic gull, seldom near land. Very delicate. There are several species of Kitiwake. They nest on tiny ledges on vertical cliffs in Norway or Alaska.
Ivory Gulls: These nest in the far north and rarely come south. They spend much time in the dark.
Migration: Nanotechnology is making devices sufficiently tiny to place geolocators on birds, which allows them to gather more information on their migration. They have a light sensor.
These sensors allowed us to gather interesting data on Sooty Sheerwaters: These come from the South in the non-breeding season. These birds go 40,000 miles per year (average of 500 miles/day). They dive up to 70 meters, particularly in the south-little activity near the equator. Another bird, the Bar-tailed Godwit, was tracked, and the data revealed that they traveled from Alaska to New Zealand without resting on the water. They flew, not resting, 7,300 miles non-stop (up to 9 days). (Note: there are birds going over the ocean that aren’t seabirds!)
Conservation and population threats:
• Global warming and climate change
• Large colonies can be especially vulnerable to oil spills
• Fishing nets and long-line hooks
• Chemical contamination of eggs
• Introduced mammalian predators
• Egg and bird collecting
What you can do:
• Join a bird conservation group
• Manomet Bird Observatory
• Puffin Project
• Support USFWS, they manage refuges that protect seabird colonies
• Join a bird conservation group
• Manomet Bird Observatory
• Puffin Project
• Support USFWS, they manage refuges that protect seabird colonies
Isles of Shoals Terns Restoration Project
Visit to Appledore Island
The Secret Life of Turtles
Presentation
• Turtles are reptiles, not amphibians (Reptiles include: turtles, crocodiles and birds, sqamalates (lizards and snakes)
• They are the oldest and most primitive of living reptiles; at least 200 million years old
• Sheels (carapace and plastron) unique in vertebrates
• Ectotherms seasonal activity cycle (April-October)
• High adult survivorship, can live almost as long as we do
• Low egg and juvenile survivorship
• Many populations are threatened
• Ectotherms: An organism whose body temperature is controlled by the outside environmental temperature
• Amphibians; moist or dry skin; no scales or claws
• Reptile has dry skin, scales and claws
• Turtles are remarkable
o The shoulder girdle and neck are inside the rib cage
o Some can live as long as humans
o Can live many days underwater without oxygen
o Can survive formonths underwater without respiratory breathing
o Can survive for months at temperatures near freezing; box turtles can actually freeze solid
o Females can store sperm for a year or more
o Can reproduce as senior citizens
o Gender of hatchlings is determined by incubation temperature, not by sex chromosomes
o Earliest turtles had teeth; now they just have beaks
o A common ancestor gave rise to lungfish, reptiles, mammals
o Slow development & unlimited growth
o Delayed sexual maturity
o No territoriality
o Variable clutch size
o Temperature-dependent gender determination
o No parental care “makes it easier if you are laying eggs your whole life”
o Hatchlings often “overwinter” in nest (survival adaptation—emerge at auspicious moment)
o Shell itself is bone
o Scutes—horny scales made of keratin--overlay bones and hold them together
o There are muscles attached to the hinge, as with bivalves, that contract when they are threatened and make them impossible to get into
o New England Turtles: about a dozen (excluding sea turtles)
o Threats
Habitat destruction
Cars
Increase in diseases (a rhonovirus has “jumped” from amphibians to box turtles, and it is very deadly
• Turtles are reptiles, not amphibians (Reptiles include: turtles, crocodiles and birds, sqamalates (lizards and snakes)
• They are the oldest and most primitive of living reptiles; at least 200 million years old
• Sheels (carapace and plastron) unique in vertebrates
• Ectotherms seasonal activity cycle (April-October)
• High adult survivorship, can live almost as long as we do
• Low egg and juvenile survivorship
• Many populations are threatened
• Ectotherms: An organism whose body temperature is controlled by the outside environmental temperature
• Amphibians; moist or dry skin; no scales or claws
• Reptile has dry skin, scales and claws
• Turtles are remarkable
o The shoulder girdle and neck are inside the rib cage
o Some can live as long as humans
o Can live many days underwater without oxygen
o Can survive formonths underwater without respiratory breathing
o Can survive for months at temperatures near freezing; box turtles can actually freeze solid
o Females can store sperm for a year or more
o Can reproduce as senior citizens
o Gender of hatchlings is determined by incubation temperature, not by sex chromosomes
o Earliest turtles had teeth; now they just have beaks
o A common ancestor gave rise to lungfish, reptiles, mammals
o Slow development & unlimited growth
o Delayed sexual maturity
o No territoriality
o Variable clutch size
o Temperature-dependent gender determination
o No parental care “makes it easier if you are laying eggs your whole life”
o Hatchlings often “overwinter” in nest (survival adaptation—emerge at auspicious moment)
o Shell itself is bone
o Scutes—horny scales made of keratin--overlay bones and hold them together
o There are muscles attached to the hinge, as with bivalves, that contract when they are threatened and make them impossible to get into
o New England Turtles: about a dozen (excluding sea turtles)
o Threats
Habitat destruction
Cars
Increase in diseases (a rhonovirus has “jumped” from amphibians to box turtles, and it is very deadly
Turtles, Part II
Chris described some common turtles, and his work at Jug Bay

• The Red-bellied Turtle (right) is almost as large as a Snapping Turtle; it has a pink-tinted shell, is ve
ry sturdy, and weighs up to 4500 g. It's primarily herbivorous (more carnivorous when young). There is a small, endangered population in Plymouth MA; a gap between this population and others residing more southerly may, it’s theorized, be due to over-hunting by Native American populations. They only come to land long enough to nest.
• Eastern Mud Turtle: A small, nondescript, bland turtle. All have a musk gland near their rear legs that is very smelly. They are very small. A roughened patch on the inner rear thighs and longer tails allow for identification of the male.
• The Red-bellied Turtle (right) is almost as large as a Snapping Turtle; it has a pink-tinted shell, is ve
ry sturdy, and weighs up to 4500 g. It's primarily herbivorous (more carnivorous when young). There is a small, endangered population in Plymouth MA; a gap between this population and others residing more southerly may, it’s theorized, be due to over-hunting by Native American populations. They only come to land long enough to nest.
• Eastern Mud Turtle: A small, nondescript, bland turtle. All have a musk gland near their rear legs that is very smelly. They are very small. A roughened patch on the inner rear thighs and longer tails allow for identification of the male.
• Common Musk Turtle, aka “The Stinkpot”
• Spotted Turtles reside into the north, up into Canada, which is unusual.

• Spotted Turtles reside into the north, up into Canada, which is unusual.
• Diamond-backed Terrapin (left) can live in salty water; they are now protected from commercial harvest.
• Bog Turtle is tiny, to 11.4 cm. It is only found in 4 northern Maryland, and is federally protected. It is not doing very well due to habitat destruction.vest.
Jug Bay on the Patuxent River
• Box Turtle census plots
• Hoop trapping sites
• Red-bellied Cooter nesting areas
• There are many volunteers; undergraduate students come in the summertime. They study overall biology to add to the knowledge base on these animals: nesting, eating habits, etc.
o Foraging
o Where they nest
o Where they overwinter
o Diet (adult)
o Local population status
o Regional status
• Methods:
o Hoop traps: all students learn how to use these
o Radio telemetry: great way to study habitat use and movements of individuals—lets them get to know each turtle as an individual
• Females have a very large home range (avg 8 hectares); males have a much smaller one (under 2 hectares); juvenile smallest (around 1 hectare)
• Radio telemetry allowed them to track a juvenile turtle quite some distance from its birthplace (juvenile dispersal)
• Juveniles probably have a higher rate of mortality than adults
• Disease is appearing in a few
Red-bellied Turtle photo from statesymbolsusa.org
Diamond-backed Terrapin photo from msa.md.gov
• Hoop trapping sites
• Red-bellied Cooter nesting areas
• There are many volunteers; undergraduate students come in the summertime. They study overall biology to add to the knowledge base on these animals: nesting, eating habits, etc.
o Foraging
o Where they nest
o Where they overwinter
o Diet (adult)
o Local population status
o Regional status
• Methods:
o Hoop traps: all students learn how to use these
o Radio telemetry: great way to study habitat use and movements of individuals—lets them get to know each turtle as an individual
• Females have a very large home range (avg 8 hectares); males have a much smaller one (under 2 hectares); juvenile smallest (around 1 hectare)
• Radio telemetry allowed them to track a juvenile turtle quite some distance from its birthplace (juvenile dispersal)
• Juveniles probably have a higher rate of mortality than adults
• Disease is appearing in a few
Red-bellied Turtle photo from statesymbolsusa.org
Diamond-backed Terrapin photo from msa.md.gov
Biogeochemical Cycles
Marilyn continued to discuss her work with isotopes. Presentation
Stable Isotope Lesson #3:Photosynthesis: Plants have lighter carbon isotopes because the lighter ones react faster.
Stable Isotope Lesson #4: Two groups of plants: C3 (vegetables, trees, rice) and C4 (corn, sugar, cane, grasses)—they each have a completely different isotope value, because inside the plant there is something different going on. C4 plants have not been around as long.
Global Biogeochemical Carbon Cycle: Everything that you depend on has to come from a biogeochemical cycle.
Chart of past cycles: Every time the biogeochemical cycle goes down, there is an ice age. So why are we worried? This has been going on for hundreds of thousands of years . . . but suddenly, things changed and it went up.
What’s the difference between global change and global warming? Marilyn discussed her research in Australia.
Megafauna were everywhere before humans arrived. Early humans burned the landscape—repeatedly. With burning, eventually the plants die completely. Ecosystem change is apparent over time in Australia 5,000 years after humans arrived. Marilyn and her colleagues gathered eggshells and analyzed the carbon isotopes. Even without fossil fuels, humans wiped out the megafauna. Animals whose vital food sources were eliminated went extinct. Emus survived; Genyornis went extinct (theory—due to burning and hunting). Ecosystem change has been much more rapid due to human activity.
Earth’s carbon cycle changed dramatically over time: when the earth formed, there was no atmospheric oxygen. Where did the Earth’s water come from? Marilyn will be publishing a paper in Science magazine about this. When the Earth formed, asteroids collided that had lots of water, creating the basis for life-supporting conditions.
Where do humans disrupt the water cycle? Light isotopes evaporate up into clouds; heavy ones rain down—“the whole earth breathing.” Humans have disrupted the biogeochemical nitrogen cycle.
Stable Isotope Lesson #4: Two groups of plants: C3 (vegetables, trees, rice) and C4 (corn, sugar, cane, grasses)—they each have a completely different isotope value, because inside the plant there is something different going on. C4 plants have not been around as long.
Global Biogeochemical Carbon Cycle: Everything that you depend on has to come from a biogeochemical cycle.
Chart of past cycles: Every time the biogeochemical cycle goes down, there is an ice age. So why are we worried? This has been going on for hundreds of thousands of years . . . but suddenly, things changed and it went up.
What’s the difference between global change and global warming? Marilyn discussed her research in Australia.
Megafauna were everywhere before humans arrived. Early humans burned the landscape—repeatedly. With burning, eventually the plants die completely. Ecosystem change is apparent over time in Australia 5,000 years after humans arrived. Marilyn and her colleagues gathered eggshells and analyzed the carbon isotopes. Even without fossil fuels, humans wiped out the megafauna. Animals whose vital food sources were eliminated went extinct. Emus survived; Genyornis went extinct (theory—due to burning and hunting). Ecosystem change has been much more rapid due to human activity.
Earth’s carbon cycle changed dramatically over time: when the earth formed, there was no atmospheric oxygen. Where did the Earth’s water come from? Marilyn will be publishing a paper in Science magazine about this. When the Earth formed, asteroids collided that had lots of water, creating the basis for life-supporting conditions.
Where do humans disrupt the water cycle? Light isotopes evaporate up into clouds; heavy ones rain down—“the whole earth breathing.” Humans have disrupted the biogeochemical nitrogen cycle.
Centennial Resurvey of the San Jacinto Mountains

Chris & Marilyn-- Centennial Resurvey of the San Jacinto Mountains, California
This family project is a whole-family venture, including ancestors! The goal is to look at a mountain range, and reveal how the wildlife have changed over the years.
Chris: Joe Grinnell was a collector, author, and museum director. Harry Swarth, Chris’ grandfather, worked with him. Many specimens were collected and preserved. All the information is online along with field notes, which were so complete that it’s possible to go back to the exact sites they visited. Left a legacy of studies that show that certain species are found in certain zones at certain elevations and are also different on the east and west sides of the mountain. Highest point, San Jacinto Peak: 10,834 feet high. Adjacent to “serious desert.”
Some of the same palm trees are visible in contemporary photos that were there 100 years ago. Chris and his family camped—it is not all built up in the mountains! They caught/trapped birds and mammals, done exactly as they did it in 1908. For some, they only needed to collect a feather, then let them go. Organs were collected for preservation. Mountains go from a low of 750 feet.
Resurvey goals:
· Replication
· New baseline
Several species were seen to have gone extinct or are almost extirpated; about three times as many new ones have appeared.
Burrowing Owls are in terrible declines, not because of anything specific in the mountains, but as part of a wider trends. There are many urban-expanding species. At the Museum of Vertebrate Zoology, they allowed a little removal of specimen to compare.
Marilyn: Birds have experienced a change in habitat. Does elevation explain any trends in stable isotopes of carbon and nitrogen? How about trophic levels?
Everything is warmer by half to three degrees (winter-summer). There’s a general trend that it’s drier at higher elevations. Hypothesis: As the climate warms, species are going to migrate up to where the climate is cooler. A study found that a chipmunk population went up, as did the Mountain Quail. Some didn’t change or went down, so it’s not consistent.
Stable isotopes: between 1908 and 2008: There is a statistical difference in CO2 concentration effects. If we compare plants that were collected on the eastern slope from the western there is also a difference. The pollution might be blowing in from Los Angeles and impacting the west more.
Remember . . . you are what you eat PLUS . . .
- The insects are key to avian diet
- Insects were not a part of sampling in 1908, so they were not collected.
Carbon sources have changed; climate, environment or diet? These birds have shifted their trophic level upwards, which means that insects have become a more predominant food source. This raises a question about how the vegetation has changed.
Many agencies and organizations are cooperating. This project shows how important preserving collections can be. Today, scientists can use tissue from specimens to learn about relationships between species, and for conservation and understanding the impacts to species. The field notes that Grinnell and Swarth took are also very valuable. There have been no other projects to attempt so much.
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