Biology is designed for multi-semester biology courses for science majors. It is grounded on an evolutionary basis and includes exciting features that highlight careers in the biological sciences and everyday applications of the concepts at hand. To meet the needs of today’s instructors and students, some content has been strategically condensed while maintaining the overall scope and coverage of traditional texts for this course. Instructors can customize the book, adapting it to the approach that works best in their classroom. Biology also includes an innovative art program that incorporates critical thinking and clicker questions to help students understand—and apply—key concepts.

By the end of this section, you will be able to:Describe the effects of abiotic factors on the composition of plant and animal communities in aquatic biomesCompare and contrast the characteristics of the ocean zonesSummarize the characteristics of standing water and flowing water freshwater biomes

In this activity, students use real water chemistry data and descriptive statistics in Excel to examine primary productivity in an urban estuary of the Salish Sea. They will consider how actual data do or do not support expected annual trends.

In this activity, students use real water chemistry data and descriptive statistics in Excel to examine primary productivity in an urban estuary of the Salish Sea. They will consider how actual data do or do not support expected annual trends.

Activities offer students the opportunity to learn about multiple facets of waterbodies and pollution, including aquatic life (indicator species), local concerns, and public outreach through research, teamwork, and role-playing exercises.

For students that have already been introduced to the water cycle this lesson is intended as a logical follow-up. Students will learn about human impacts on the water cycle that create a pathway for pollutants beginning with urban development and joining the natural water cycle as surface runoff. The extent of surface runoff in an area depends on the permeability of the materials in the ground. Permeability is the degree to which water or other liquids are able to flow through a material. Different substances such as soil, gravel, sand, and asphalt have varying levels of permeability. In this lesson, along with the associated activities, students will learn about permeability and compare the permeability of several different materials for the purpose of engineering landscape drainage systems.

Los estudiantes miran un video, leen el cuadernillo y usan su experiencia propia para escribirle a sus amigos, una carta con informacion que contesta la pregunta: "¿Qué es un estuario y qué lo hace tan especial?" Cuadernillo de lectura que acompaña la tarea de desempeño.

Puerto Rico's San Juan Bay Estuary faces multiple threats, including heavy use by urban populations and impacts of climate change. A workbook from the EPA's Climate Ready Estuaries program helped them catalog, prioritize, and address their climate risks.

This resource is a video abstract of a research paper created by Research Square on behalf of its authors. It provides a synopsis that's easy to understand, and can be used to introduce the topics it covers to students, researchers, and the general public. The video's transcript is also provided in full, with a portion provided below for preview:

"Fresh water flows from rivers to estuaries and then to the sea, creating a salinity gradient as it meets the salt water of the ocean. While this salinity gradient is likely to have profound effects on the organisms that call these habitats home, its impact on microbial communities is far from clear. To fill this gap, researchers recently used genomic, transcriptomic, and geochemical data to examine microbial variation in both benthic and planktonic environments along a river-to-sea continuum. They observed a distinct increase in osmoregulation-related gene expression with increasing salinity and noted a prevalence of phosphate-acquisition activities among microorganisms inhabiting the freshwater zone, likely resulting from phosphate limitation, while carbon-, nitrogen-, and sulfur-cycling processes became dominant in brackish water, due to higher nutrient levels. In these brackish waters, photosynthesis was mainly conducted by cryptomonads in the water column and diatoms in the sediment..."

The rest of the transcript, along with a link to the research itself, is available on the resource itself.