Asking Questions in Biology

CONTENTS OF CURRICULUM UNIT 26.06.04

  1. Unit Guide
  1. Introduction/rationale
  2. Demographics
  3. Content Objectives 
  4. Teaching Strategies
  5. Classroom Activities
  6. Resources
  7. Annotated Bibliography
  8. Appendix On Implementing District Standards
  9. Notes

Questions to Discoveries, Exploring Temperate Grasslands and Temperate Forests

Stacy-Ann Morrison Thomas

Published September 2026

Tools for this Unit:

Content Objectives 

Living in Delaware gives students many opportunities to get up close and personal with nature. The very tall deciduous trees that are home to the birds chirping from the forest canopy, the mushrooms growing on huge fallen logs, and streams that support a variety of fish, amphibians, and aquatic insects are all visible during an evening stroll through the White Clay Creek State Park or Brandywine Creek State Park. Students may find themselves in wide meadows where grasses predominate and butterflies, bees, and other pollinators thrive after taking a little trip past these woodlands. Despite their apparent differences, all habitats have one crucial thing in common: they are living systems where creatures constantly interact with the nonliving environment and each other. These interesting observations about the natural world give rise to one of the essential questions that help to guide the development of this curriculum unit: How does climate shape life in grassland and temperate forest biomes?

Biomes and Ecosystems

What makes some parts of the Earth thrive with endless grasslands while other parts are filled with a variety of towering trees? To answer this question, we will take a closer look at the factors that shape these biomes. These factors include climate, soils and seasons, human activity, and environmental factors such as fire frequency. As we consider the possible responses to this question and others, it is important to step back and focus on the bigger picture to understand the basics of biome, ecosystem and habitat. According to the National Geographic Society, scientists currently disagree on what makes up a biome; however, it is argued that biomes are typically characterized by the resident biota within them and the climate that drives the area.[3] Biota refers to all the plants (flora) and animals (fauna) living within a biome that are adapted to the conditions. Biomes differ by the climate, soil type and the types of organisms that live in the area. The area itself can extend thousands of square miles and span across continents. There are several types of biomes, for example, tropical rainforest, temperate forest, desert, tundra and grassland. Each biome has its own distinct climate, animal community and plant life. In this unit, the focus will be on both temperate grasslands and temperate forests.

To better frame the topic, it must be established that biomes differ from ecosystems and habitats, as these terms are generally misused. This can compromise scientific information and meaningful scientific discourse. While biomes are the larger geographical areas, within them are more localized geographical ecosystems, which are communities of organisms interacting with their physical environments (biotic and abiotic components).[4] Abiotic components include water, soil, atmosphere, temperature, etc. Biotic components refer to the living organisms in the ecosystem or anything that was once alive. Examples of ecosystems are rivers, freshwater lakes and deserts. Within ecosystems, there are even more localized areas called habitats. A habitat is an organism’s home that supports its needs; it is where they reside. For example, a polar bear has a habitat in the Arctic where it hunts for seals on ice, while a kangaroo has a habitat in the Australian outback. Habitats are organism‐specific and relate to the presence of a species, population, or individual animal or plant to an area's physical and biological characteristics. Habitat implies more than vegetation or vegetation structure; it is the sum of the specific resources that are needed by organisms.[5]

As students continue to learn more about biomes, it is important to recognize that they can differ significantly based on their region or where they are located geographically. Biomes exhibit distinct climates and support a variety of different plants and animals that may be unique to that particular biome. These regional differences influence the biodiversity and human interaction with these environments. For example, grasslands in different parts of the world such as Africa, Asia or South America are not all identical. They may share similar defining characteristics such as open landscapes dominated by grasses and relatively few trees, but each has its own communities of flora and fauna. Biodiversity refers to the variety of life on Earth. It includes variation at all levels of biological organization, from the genetic variation within a single population or species to the species living in a particular ecosystem and the communities of ecosystems that make up a biome or the entire biosphere.[6] Biodiversity contributes to a healthy and resilient ecosystem. Students will better understand this concept by explaining a scenario about pollinators such as bees, butterflies or birds and their role in the environment. An abundance of these pollinators will result in increased flowering plant reproduction, as organisms that depend on these plants will benefit significantly and ultimately the entire food web is stronger. Any small change in a single species can affect balance and have a rippling effect through the entire food web. Students will then understand and recognize that protecting every organism, regardless of their size, is significantly important since it can have ecological implications.

For students to fully understand the importance of biodiversity, they will need to have an understanding of ecology. Ecology is the scientific study of the distribution and abundance of organisms and the interactions both with each other and with their physical environment.[7] It focuses on the study of the ecosystem, and so an ecologist may choose to explore a single predator-prey relationship or an entire biome and how these organisms may interact with each other and with the environment. Imagine a pocket gopher living in a temperate grassland or a European badger who lives in the temperate forest; they certainly do not live in isolation. They eat the vegetation and seeds, aerate the soil by digging tunnels through it and create homes for other animals that live in it. They also serve as food or prey for predators such as hawks, foxes and coyotes. This creates balance in the environment as the soil benefits tremendously from it being fertilized due to the introduction of organic matter as the soil turns. An abundance of plants will be able to grow, which then provides food and serves as a home to various organisms. Here we see how interactions can determine abundance.

The Grassland Biome

With a deeper understanding of predator-prey relationships and how it shapes an ecosystem, students will now learn more about the grassland biome with a focus on temperate grassland. Students will also be exposed briefly to the other types of grassland for comparison, such as tropical and montane grasslands.  In general, Grasslands are biological communities containing few trees or shrubs, distinguishable by their vast, concentrated ground cover of mixed herbaceous vegetation dominated by grasses.[8] Grasslands vary greatly and can be found on every continent across the world. They differ widely in climate, vegetation, soil profiles and animal life. For instance, there are the temperate grasslands that represent one of the Earth's major biomes; they are largely treeless and historically have been one of the most productive and diverse terrestrial biomes. Temperate grasslands are predominantly located in the Northern Hemisphere, stretching across vast regions of North America, South America, Eurasia, Africa, and Oceania.[9] Temperate grasslands are often referred to by different names and vary in size. The larger temperate grasslands include prairies in the United States and Canada, pampas found in Argentina and Uruguay, steppes in Russia and Central America as well as the veldts in South Africa. These generally experience extreme seasonal temperatures with hot summers and extremely cold winters. There are smaller grasslands found in Hungary, which is called puszta and the downs and tussock found in Australia and New Zealand.

In contrast, tropical grasslands, which are also called savannas, remain warm all year round but often experience dramatically wet and harshly dry seasons alternately. This gives rise to the growth of drought-resistant trees, which grow sparsely among tall grasses when compared to temperate grasslands that are treeless due to climate conditions. A few tropical grasslands are the Serengeti (East Africa), the Cerrado (Brazil), and the Northern Australian Savannas. While the overarching definition of a tropical grassland highlights its seasonal climate, exploring specific regional variations such as the mammalian-dominated Serengeti or the fire-adapted Cerrado shows how complex these open landscapes truly are.[10] The long-term distribution and stability of tropical savannas depend heavily on the dynamic interactions between highly seasonal rainfall, soil nutrient availability, recurring wildfires, and intense herbivore grazing.

While the other grasslands differ greatly in climate, vegetation and animal species, montane grassland presents another set of climate and ecological adaptations. They are characterized by cool temperatures, thin soil layers, and unique plant and animal life. Montane grasslands are found at extremely high elevations in mountains, beneath the snowline but above the tree line. Because it is too windy and cold for trees to survive at this elevation, grasses take over.[11] Located high in the northern Andes Mountains of South America, the páramo is the best-known example. Millions of people who live downstream receive water from its moist, spongy soil, which absorbs rain and snowfall like a sponge and gradually releases it into rivers.[12] Because the páramo is a relatively young ecosystem, having only formed in the last two to three million years when the Andes became tall enough to support it, scientists have also discovered that páramo plants change into new species more quickly than plants in nearly every other location on Earth.[13] Many of the flora and animals that inhabit alpine grasslands like this are unique to the globe because they are dispersed and isolated, resembling islands in the sky.[14]

How Climate Influences Temperate Grasslands

The defining climatic feature of temperate grasslands is contrast. Summers are hot, winters are cold, and the annual swing between the two is much sharper than in tropical grasslands.[15] Annual precipitation is moderate, generally somewhere between 25 and 89 centimeters (roughly 10 to 35 inches) per year, which is enough to support dense grass cover but too little, combined with periodic drought, to allow most trees to establish and survive.[16] This precipitation total also varies meaningfully across the biome and directly shapes what kind of grassland forms: wetter regions closer to 75–89 cm of rain tend to grow tall, dense grasses, while drier regions produce shorter, sparser grass cover. In North America, this gradient produces a recognizable pattern moving west to east, from short-grass prairie in the rain-shadow of the Rocky Mountains to mixed-grass and finally tall-grass prairie in the wetter eastern Great Plains.[17]

This climate does more than determine grass height. The same conditions that limit tree establishment, temperature extremes, seasonal drought, and periodic fire, also actively maintain the open character of the grassland once it forms. In other words, temperate grasslands are not simply places where trees have not yet grown; they are actively held in a grass-dominated state by recurring disturbance.[18] The climate of a temperate grassland doesn't just decide how tall the grass grows, it actually keeps the whole landscape from turning into a forest. The three influences are extreme hot and cold temperatures, dry spells during the growing season, and fires that sweep through every few years. Each of these factors makes life hard for tree seedlings, in particular. Grasses can survive extreme heat and cold, bounce back after drought, and regrow quickly after a fire because most of their living tissue is safely underground in their roots. However, young trees can't do any of this nearly as well. Their seedlings are far more likely to dry out, freeze, or burn before they will ever grow tall enough to survive on their own. This is why it is not accurate to think of a grassland as just an empty space where a forest simply has not grown in yet, as if trees are on their way and just haven't arrived. A grassland isn't "unfinished." It's an ecosystem that gets renewed again and again by the same harsh conditions that would kill off any trees trying to take root. Take away the fires, or the droughts, or the temperature swings, and over time trees and shrubs would likely move in and the grassland would slowly disappear. Hence, the "openness" of a grassland, the fact that it's mostly grass with few or no trees, is not an accident, a coincident or a pause. It's something the environment is actively maintaining, year after year, through repeated stress and disturbance.

Fertile Soils of Temperate Grasslands: The Mollisol Advantage.

The significance of temperate grasslands to human civilization may be best explained by their soil. Soil is a natural resource characterized by the thin layer covering the entire earth's surface, except for open water surfaces and rock outcrops. The properties of soil are determined by environmental factors. Five dominant factors are often considered in the development of the various soils: (a) the climate, (b) parent materials (rocks and physical and chemical derivatives of same), (c) relief, (d) organisms (fauna and flora), and (e) the time factor.[19] This biome's distinctive soil is a member of the Mollisols soil order, which derives from the Latin mollis, which means "soft." A deep, black, organic-rich surface layer known as a mollic epipedon, which can extend 60 to 80 centimeters below the surface and is formed by a process known as melanization. The gradual darkening of soil brought on by the decomposition of organic matter is what defines mollisols.[20] Because grasses have a disproportionate amount of their biomass underground, this dark layer accumulates. Their vast, fibrous root systems, which can extend 1 to 2 meters (3 to 6 feet) into the soil, become dormant and then sprout periodically, continuously depositing organic material below ground.

Over time, burrowing creatures like earthworms, ground squirrels, and prairie dogs deepen and enrich the mollic epipedon by mixing this organic debris further into the soil profile. The end product is some of the most readily cultivated, naturally productive soil on the planet. Despite making up only 7% of the world's ice-free land area, mollisols constitute the foundation of the United States' "breadbasket" agricultural regions. This fertility is a double-edged sword for the biome.[21] This means that the same fertility which makes the mollisol so productive and valuable comes with great risks. Due to the fertility of this rich soil, it results in it being heavily farmed, which can lead to soil degradation, erosion and loss of long-term productivity. It is a benefit but it also requires careful management to avoid exhausting the soil. Temperate grasslands have been the focus of extensive agricultural conversion more than almost any other biome due to the same characteristics that made these soils so appealing to ancient grasses and grazing animals.

Vegetation and Plant Adaptations.

Grasses are not simply the tallest plants that happen to survive in this biome; they are highly adapted to it. Two broad growth strategies coexist across temperate grasslands: sod-forming grasses, which spread laterally through underground stems called rhizomes and create dense, interlocking turf, and bunch grasses, which lack rhizomes, reproduce by seed, and tend to dominate the drier portions of the biome.[22] Both strategies share a common defense against the biome's stresses: massive investment in root tissue relative to visible above-ground growth, which anchors plants against wind erosion, allows them to store water and carbohydrate reserves underground during drought, and lets grasses resprout quickly after fire or grazing removes their leaves. Grasses are not alone in this landscape. Interspersed among them are hundreds of species of non-woody flowering plants known as forbs, including asters, coneflowers, and blazing stars in North American prairies, that add seasonal color and floral diversity without competing directly with grasses for the same root depth. True woody plants, by contrast, are largely excluded except along rivers and streams, where increased water availability allows species like cottonwood, oak, and willow to survive despite the biome's otherwise unfavorable conditions for trees. [23]

Disturbance Ecology: Why Fire and Grazing Matters.

One of the most important ideas about temperate grasslands is that they need to be disturbed to stay healthy. Without regular fires and grazing animals, most temperate grasslands would slowly turn into shrubland or forest over time. Fire has always been part of this system. Long ago, lightning started most fires, and for thousands of years afterward, Indigenous peoples also set fires on purpose. These fires burn away dead grass and plant litter, put nutrients back into the soil, and kill young trees and shrubs before they can grow big. Grasses survive these fires just fine because their roots stay safe underground and can quickly grow new leaves afterward.[24]

Grazing by large herbivores works alongside fire rather than replacing it. In North America's tallgrass prairie, research at sites such as the Konza Prairie Biological Station and the Tallgrass Prairie Preserve has shown that reintroduced bison (Bison bison) create a patchwork of grazed and ungrazed, burned and unburned areas, and this patchiness, rather than uniform grazing pressure, is what supports high biodiversity. Bison also physically disturb the ground through wallowing, rolling in dust to control insects and shed fur, which creates bare-soil depressions that become colonized by different, often short-lived plant species than the surrounding turf, adding yet another layer of habitat variety to the landscape. Studies tracking insects such as grasshoppers and ground beetles across burned and grazed prairie plots have found that this combination of fire frequency and bison grazing significantly increases species diversity and evenness compared to areas managed with only one disturbance type or none at all. Even grassland birds respond to this mosaic: species like the Henslow's sparrow and upland sandpiper favor different combinations of recent fire and grazing intensity, meaning that a variable, patchy disturbance regime supports a wider range of bird species than a uniform one.[25]

The Temperate Forest Biome

Unlike grasslands, temperate forests receive abundant rainfall throughout the year, allowing trees to become the dominant vegetation. Temperate deciduous forests are characterized by four distinct seasons, with warm summers, colorful autumns, cold winters, and mild springs. This seasonal cycle influences every aspect of life within the forest. One of the defining features of temperate forests is the presence of deciduous trees such as oaks, maples, beeches, and hickories. During autumn, these trees shed their leaves in preparation for winter. This adaptation allows trees to conserve water and energy when temperatures decrease and sunlight becomes less available. In spring, new leaves emerge, allowing photosynthesis to resume and supporting another season of growth.[26]

The layered structure of temperate forests creates numerous habitats within a relatively small area. The canopy receives the greatest amount of sunlight and provides habitat for birds, squirrels, and insects. Beneath the canopy, smaller trees and shrubs occupy the understory, while the forest floor supports fungi, mosses, insects, worms, and countless decomposers responsible for recycling nutrients.[27] Students are often fascinated by the idea that fallen leaves are not simply waste but rather an essential part of the ecosystem. As decomposers break down dead plant material, nutrients are returned to the soil, where they become available for new plant growth. This continuous recycling of matter demonstrates one of the fundamental principles of ecology: ecosystems depend upon the cycling of energy and nutrients to remain healthy. Temperate forests support tremendous biodiversity because they provide a variety of habitats and food sources. Deer browse on shrubs and young plants, while black bears consume berries, insects, fish, and small mammals. Woodpeckers remove insects from tree bark, helping maintain forest health, while salamanders, frogs, and countless invertebrates thrive within moist leaf litter. Each organism contributes to the overall functioning of the ecosystem.

Temperate Forest Location and Climate.

Temperate forests are mostly found in the mid-latitudes, approximately between 25° and 50° north and south of the equator, primarily in eastern North America, Western and Central Europe, and East Asia, smaller pockets can be found in southern Chile and southeastern Australia.  Nearly all of the world's temperate deciduous forests are located in this region. In contrast to temperate grasslands, with limited moisture and frequent disturbance, temperate forests receive consistent annual precipitation.[28] Usually around 30 to 60 inches or 750–1,500 mm throughout the year, although not universal. This precipitation is distributed fairly evenly throughout the year and is considered a highly dependable water supply, which allows trees to meet the high moisture demands required to grow tall trunks, extensive root systems, and broad canopies, making forests the dominant vegetation in these regions.[29][30]

Temperate forests experience the four distinct seasons, spring, summer, autumn, and winter, which shape nearly every aspect of the ecosystem. The summers are generally warm and wet, while winters are cold and often snowy which creates a period where plants grow approximately 120 to 250 days followed by a dormant period. This seasonal cycle drives many of the adaptations seen in temperate forests.[31] Deciduous trees such as oaks, maples, beeches, and hickories shed their leaves each autumn to conserve water and energy during the colder months when sunlight is limited. In spring, the trees showcase new leaves emerging, once again photosynthesis resumes, and another flourishing season where growth begins. The combination of reliable rainfall and pronounced seasonal change distinguishes temperate forests from grasslands and supports the rich biodiversity characteristic of this biome, setting it apart from other biomes.[32][33]

Temperate Forest Vegetation and Layered Structure

Temperate forests are generally classified into three major types: temperate deciduous forests, temperate coniferous forests, and temperate rainforests. Although all occur within temperate regions, they differ in climate, dominant vegetation, and annual precipitation. Deciduous forests experience distinct seasons and are dominated by broad-leaved trees, such as oak, maple, beech, birch, and hickory, that lose all their leaves for part of the year, while coniferous forests provide year-round greenery and shelter for various species. They include needle-leaved evergreen trees like pine, fir, and spruce, which usually dominate a given region depending on local temperature and moisture conditions. The deciduous forests are the most common type across eastern North America, Europe, and East Asia. Temperate rainforests, found in regions with exceptionally high annual precipitation, support towering coniferous trees, dense understory vegetation, and abundant mosses and ferns.[34][35]

Rather than growing in a single uniform layer, a temperate forest organizes itself into distinct vertical layers, each with its own light levels, humidity, and resident species. At the top sits the canopy, made up of the tallest, dominant trees, whose leaves capture most of the available sunlight and cast shade over everything below. Beneath that is the understory, composed of smaller, shade-tolerant trees and saplings waiting for an opening in the canopy above. Below the understory is the shrub layer, made up of woody, multi-stemmed plants such as dogwood and blueberry that can survive on the reduced light filtering down from above, and beneath that, the herbaceous or ground layer, home to wildflowers, ferns, and mosses adapted to deep shade. Finally, the forest floor itself is covered in leaf litter, fungi, and decomposing organic matter, which breaks down to make temperate forest soils some of the most fertile in the world.[36]

The defining plant adaptation in this biome is deciduous leaf drop. As temperatures fall in autumn, trees stop producing chlorophyll, the green pigment used in photosynthesis, which allows other pigments already in the leaf to show through as the reds, oranges, and yellows of fall color, before the tree seals off and sheds its leaves entirely. This isn't simply leaves dying from cold; it's an active survival strategy.[37] By dropping leaves that would otherwise freeze, tear in winter storms, or lose water the tree can't replace from frozen ground, deciduous trees conserve energy and avoid damage through the coldest months, then regrow a fresh canopy each spring when conditions improve.

Temperate Forests: Animal Life and Food Webs

Just as temperate forest plants have evolved to cope with a hard seasonal boundary, so have the animals that live among them, and their strategies generally fall into three categories: hibernation, migration, and camouflage. Hibernation allows animals like black bears and groundhogs to slow their metabolism dramatically and sleep through the winter months when food is scarce, while some smaller animals, such as chipmunks and certain ground squirrels, rely instead on caching, or hoarding, the food they gathered in autumn to eat gradually through winter without fully hibernating. Migration solves the same problem differently, many forest birds, including robins, warblers, and other songbirds, fly south each fall to reach areas with more available food, then return north each spring to breed. Camouflage is a year-round strategy where the animals blend in with their environment to reduce visibility, making it difficult for predators to detect them.[38] For example, the reddish-brown coat of a white-tailed deer blends into fallen leaves and tree bark, helping it avoid predators. Some animals are also able to change their color seasonally to match snow cover in winter and green or brown vegetation in summer.

These adaptations connect into a single, interlocking food web. In an Appalachian deciduous forest, for example, oak and hickory trees produce acorns and nuts that feed seed-caching animals like squirrels and chipmunks; those small mammals, along with insects and amphibians on the forest floor, in turn support mid-level predators such as foxes and owls; while apex predators like black bears and, in areas where they've been reintroduced, wolves, help keep deer and smaller mammal populations in check. Every level of this food web, from the trees at the canopy down to the fungi and insects decomposing leaf litter on the forest floor, is tied to the same seasonal rhythm of growth, dormancy, and regrowth, temperate forest biodiversity depends on the whole system moving through its yearly cycle together.[39]

Human impact and the Importance of Conservation.

While temperate grasslands experience moderate rainfall with hot summers and cold winters, which reduces plant growth and affects grazing animals that depend upon grasses for food, temperate forests experience warmer winters, earlier springs, and increased outbreaks of insect pests that damage trees. Some species usually migrate into new regions while others decline due to the unavailability of suitable habitat. These changes illustrate one of ecology's most important principles: altering one part of an ecosystem often affects many other components. As human activities continue to alter the natural landscapes, many conservation efforts are in motion to help protect grassland and temperate forest biomes. National parks, wildlife refuges, conservation easements, and habitat restoration projects preserve important ecosystems while providing opportunities for scientific research and environmental education. Restoration projects often involve removing invasive species, replanting native vegetation, restoring wetlands, and using prescribed burns to maintain healthy grassland ecosystems.[40][41] These efforts demonstrate that humans can play a positive role in protecting biodiversity when scientific knowledge guides environmental decision-making. Conservation also begins with individual actions. Middle school students may feel that environmental problems are too large for them to influence, but small actions can collectively make a meaningful difference. Recycling, reducing waste, planting native species, conserving water, participating in community clean-up projects, and supporting local conservation organizations all contribute to healthier ecosystems. Encouraging students to see themselves as environmental stewards helps them understand that science is not only about learning facts but also about making informed decisions that improve the world around them.

Conclusion: From Questions to Discoveries

The story of grasslands and temperate forests is, in many ways, the story of scientific inquiry itself. Early observers asked simple descriptive questions such as why does this place look different from the other or how do the weather and the plants in this Biome help it stay balanced and support the animals that live in it? In teaching this unit, students are invited to exercise their curiosity and formulate their own questions. Over generations, ecologists refined questions into testable ones. The discoveries covered in this unit, the fertility of grassland soils, the layered structure of forest canopies, the seasonal strategies of forest animals, the fire thresholds separating grassland from forest did not emerge all at once. They accumulated across decades of careful observation, data collection, and comparative study, much like the inquiry process students are asked to practice in their own investigations. The questions that remain open, how these biomes will respond to a changing climate, how conservation can balance human land use with ecological health are the discoveries the next generation of scientists, including today's students, will be responsible for making.

An understanding of how temperate grasslands and temperate forests function and how human activities influence them will prepare students to make evidence-based decisions about environmental stewardship. By investigating these biomes through scientific inquiry, students develop a deeper appreciation of biodiversity and recognize their own role in protecting ecosystems at both local and global scales

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