ECOSYSTEM BIOGEOCHEMISTRY
Lecture 1 - Introduction ECOSYSTEM BIOGEOCHEMISTRY
Agenda | Lecture 1, Week 1 1:40 – 1:45 | Instructor Introduction 1:45 – 2:00 | Student Introduction 2:00– 2:30| Introduction to Ecosystem Biogeochemistry • History of Ecosystems and Biogeochemistry • Introduction to Systems • Introduction the Biogeochemistry of Earth’s Spheres 2:30– 3:00 | Syllabus Orientation Your guide: Dr. Rebecca R. Hernandez Your additional guides:
Dr. Pawlok Dass Louisa Rogers
Exper se: ecological modeling, earth Exper se: soil biogeochemistry, globally system science, and biogeochemistry important plant symbionts (e.g., mycorrhizal fungi), nutrient cycling Personal Introduction
> About Me
Assistant Professor Dept. of Land, Air and Water Resources, UC Davis
UC President’s Energy and Resources Group, University of California, Berkeley Postdoctoral Fellow Climate and Carbon Sciences Division, LBNL Advisor: Daniel Kammen and Margaret Torn
Ph.D. Dept. of Earth System Science, Stanford University Earth System Science PhD, Advisor: Christopher B. Field
M.S. Dept. of Biological Sciences, California State University, Fullerton Biology MS, Advisor: Darren R. Sandquist
B.A. Dept. of Geography, University of California, Los Angeles Geography BA, Emphasis: GIS and Remote Sensing Advisor: Thomas W. Gillespie
A.S. Saddleback Valley Community College Biology and Geography AS/AA, Advisor: Jane Horlings
Secrets to Post-Coursework Success While Taking Coursework
1. Attend every class and arrive at least five minutes early to meet other people and build relationships.
Secrets to Post-Coursework Success While Taking Coursework
2. Sit in front rows or seats nearest to the professor, if possible (so you don’t daydream or fall asleep).
Secrets to Post-Coursework Success While Taking Coursework 3. Plan out your week, in 30 minute increments, on Sunday night before each week in your planner. Secrets to Post-Coursework Success While Taking Coursework 4. Buy/download several books on course subject. If you don’t understand something, maybe the author just explained it poorly. Personal Introduction
> About Me
Assistant Professor Dept. of Land, Air and Water Resources, UC Davis
UC President’s Energy and Resources Group, University of California, Berkeley Postdoctoral Fellow Climate and Carbon Sciences Division, LBNL Advisor: Daniel Kammen and Margaret Torn
Ph.D. Dept. of Earth System Science, Stanford University Earth System Science PhD, Advisor: Christopher B. Field
M.S. Dept. of Biological Sciences, California State University, Fullerton Biology MS, Advisor: Darren R. Sandquist
B.A. Dept. of Geography, University of California, Los Angeles Geography BA, Emphasis: GIS and Remote Sensing Advisor: Thomas W. Gillespie
A.S. Saddleback Valley Community College Biology and Geography AS/AA, Advisor: Jane Horlings
Personal Introduction
> About Me
Assistant Professor Dept. of Land, Air and Water Resources, UC Davis
Summer at “Big UC President’s Energy and Resources Group, University of California, Berkeley Postdoctoral Fellow Climate and Carbon Sciences Division, LBNL Green” Advisor: Daniel Kammen and Margaret Torn Environmental Ph.D. Dept. of Earth System Science, Stanford University Consultant Earth System Science PhD, Advisor: Christopher B. Field Ecosystem Science M.S. Dept. of Biological Sciences, California State University, FullertonLab, UCR Biology MS, Advisor: Darren R. Sandquist
B.A. Dept. of Geography, University of California, Los Angeles Taught 3 Years at Geography BA, Emphasis: GIS and Remote Sensing CSU Advisor: Thomas W. Gillespie GIS Analyst (Non- A.S. Saddleback Valley Community College Profit) Biology and Geography AS/AA, Advisor: Jane Horlings
Math Tutor Personal Introduction
> About Me
Assistant Professor Dept. of Land, Air and Water Resources, UC Davis
UC President’s Energy and Resources Group, University of California, Berkeley Postdoctoral Fellow Climate and Carbon Sciences Division, LBNL Advisor: Daniel Kammen and Margaret Torn
Ph.D. Dept. of Earth System Science, Stanford University Earth System Science PhD, Advisor: Christopher B. Field
M.S. Dept. of Biological Sciences, California State University, Fullerton Biology MS, Advisor: Darren R. Sandquist
B.A. Dept. of Geography, University of California, Los Angeles Geography BA, Emphasis: GIS and Remote Sensing Advisor: Thomas W. Gillespie
A.S. Saddleback Valley Community College Biology and Geography AS/AA, Advisor: Jane Horlings
Aridlab | Land, Air, & Water Resources Dept.
Dr. Rebecca R. Hernandez UC Davis
The Aridlab seeks to understand, predict, and respond to anthropogenic and natural changes in aridlands from global to local scales.
www.Aridlab.org
@theHernandezLab
LAWR, UC Davis
ECOSYSTEM BIOGEOCHEMISTRY
Agenda 1:40 – 1:45 | Instructor Introduction 1:45 – 2:00 | Student Introduction 2:00– 2:30| Introduction to Ecosystem Biogeochemistry 2:30– 3:00 | Syllabus Orientation What is Ecosystem Biogeochemistry?
• An enormous, interdisciplinary field • A class to increase your conceptual understanding of biogeochemical processes on Earth • A class to learn meta-analytical techniques that can be useful for atmospheric scientists, biologists, ecologist, geologists, soil scientists, hydrologists, oceanographers interested in biogeochemical processes • A class that can provide motivational deadlines to begin writing a manuscript What is Ecosystem Biogeochemistry is not?
• A course to learn about litter bag decomposition techniques and methods (or other myopic methodologies that may be useful for 1/20th of the class participants. . .) • A course with applied chemistry problems – you will not be: – Calculating the pH of buffers – Predicting equilibrium concentrations – Calculating reaction rates Personal Introduction
> About You?
1. Name 2. Graduate Program/Undergraduate Major(s) 3. Why you are taking the class? 4. Favorite ecosystem, plant community, or species and why?
ECOSYSTEM BIOGEOCHEMISTRY
Agenda 1:40 – 1:45 | Instructor Introduction 1:45 – 2:00 | Student Introduction 2:00– 2:30| Introduction to Ecosystem Biogeochemistry 2:30– 3:00 | Syllabus Orientation What is Ecosystem Biogeochemistry?
• Ecosystem • Biogeochemistry
California State Employee (MBA): I don’t know. Something about . . . Ecosystem what? It sounds like a million different things all together.
Engineer (MS): It’s sounds like system impacts on the environment
Mom: That means, how the ecological systems relate to biological and geographical systems.
Agent Shelou (Geek Squad):
What is Biogeochemistry?
The scientific study of the chemical, physical, geological, and biological processes and reactions that govern the composition of the natural environment (including the biosphere, the hydrosphere, the pedosphere, the atmosphere, and the lithosphere), and the cycles of matter and energy that transport the Earth's chemical components in time and space.
History of the term: Gorham 1991 (DISCUSSION) What is Biogeochemistry?
• Definition is scale-independent • Homo sapiens, as a species, are increasingly impactful • For most of Earth’s history, the biogeochemistry was microbial • Microbial ecology remains understudied today but is becoming increasingly recognized (some textbooks are still catching up)
What is Biogeochemistry? What is Biogeochemistry?
Hierarchy of En es Systems, (Haila 1999) Processes
What is an Ecosystem?
Arthur G. Tansley What is an Ecosystem?
Arthur G. Tansley, founder of New Phytologist, What is an Ecosystem?
“It is the systems so formed which, from the point of view of the ecologist, are the basic units of nature on the face of the earth. Our natural human prejudices force us to consider the organisms (in the sense of the biologist) as the most important parts of these systems, but certainly the inorganic " factors" are also parts - there could be no systems without them, and there is constant interchange of the most various kinds within each system, not only between the organisms but between the organic and the inorganic. These ecosystems, as we may call them, are of the most various kinds and sizes.”
Arthur G. Tansley (1935) The use and abuse of vegeta onal concepts and terms, Ecology What is an Ecosystem?
Wikipedia | An ecosystem is a community of living organisms in conjunc on with the nonliving components of their environment (things like air, water and mineral soil), interac ng as a system.
Tansley (1934); Molles (1999), p. 482; Chapin et al. (2002), p. 380; Schulze et al. (2005); p. 400; Gurevitch et al. (2006), p. 522; Smith & Smith 2012, p. G-5
Arthur G. Tansley (1935) The use and abuse of vegeta onal concepts and terms, Ecology Biosphere
Biome
Levels of Organization Ecosystem in Ecology
(Organizational Community Complexity) Popula on
Species
Organism
Genes Biosphere: The sum of all dead and living materials on Earth
Biome
Ecosystem
Organizational Community Complexity Popula on
Species
Organism Systems
Systems thinking concerns an understanding of a system by examining the linkages and interac ons between the components that comprise the en rety of that defined system. Systems
In systems science, it is argued that the only way to fully understand why a problem or element occurs and persists is to understand the parts in rela on to the whole. • plays the foil to Descarte’s Reduc onism • Ludwig von Bertalanffy coined the term “general systems theory”
Types of Systems Types of Systems Types of Systems Types of Systems
Disclaimer: The specifica on of what types of transfers are excluded varies in the closed systems of physics, chemistry or engineering. Types of Systems
Pedosphere
Atmosphere Lithosphere
Biosphere Hydrosphere
The Earth System’s Spheres A Box Modeling of Systems
• How can we study or observe complicated systems such as the biosphere or the atmosphere? • Models – A way to keep track of matter or energy (for example – carbon, nitrogen, ozone, heat) – Used to predict (or retrodict) in the absence of complete data – Models can be either very detailed or very general – General models may yield as much valuable information as very detailed models – Trade-offs: the more detailed the model, the more time it takes to develop the model and run it – Box Models – a simple type of model Atmosphere | Regulates the Earth's climate, transports energy and matter around the planet Biosphere | The chemical engine that supplies energy and nutrients to most life on Earth Hydrosphere
The universal solvent, transport agent, H2O is essential for physiological processes Lithosphere
Comprises the hard, rigid outer layer of the Earth and subdivided into tectonic plates, reacts chemically to the atmo-, hydro-, and biosphere. Pedosphere | Foundation of terrestrial ecosystems, source of nutrients, supplies H2O, and habitat for soil organisms and vegetation. Pedosphere
Atmosphere Lithosphere
Biosphere Hydrosphere
The Earth System’s Spheres Atmosphere
Major Cons tuents (by volume) N2 (Nitrogen) | 78%, 780,840 ppm O2 (Oxygen) | 21%, 209,460 ppm
Minor Cons tuents Ar (Argon) | 1%, 9,340 ppm Water Vapor | 1%, highly variable
CO2 (Carbon dioxide) | 0.04%, 406 ppm Ne (Neon) | 0.002%, 18 ppm He (Helium) | 0.0005% ppm
Hydrosphere
Sea Water
Major Cons tuents (by volume)
H2O (Water) | 96.5%, 965,000 ppm NaCl (Sodium Chloride, Salt) | 3.5%, 35,000 ppm
Minor Cons tuents of Salt (sum to 3.5% total)
Biosphere
Human Body (% by mass)
Major Cons tuents* O (Oxygen) | 65% C (Carbon) | 18% H (Hydrogen) | 9.5% N (Nitrogen) | 3.2%
Minor Cons tuents Ca (Calcium) | 1.5% P (Phosphorus) | 1.2%
*The human body is 62% H2O (water)
Biosphere Plants (% by mass)
Major Cons tuents O (Oxygen) | 65% C (Carbon) | 18% Atmosphere H (Hydrogen) | 9.5% N (Nitrogen) | 3.2% Soil (including P (Phosphorus) | 0.75 – 1.0% microbes) S (Sulfur) | < 1.0%
Forms of Essential Elements Taken up by Plants
Refresh: The superscript refers to the net charge of the ion. Ions are atoms or molecules that have gained or lost one or more valence electrons giving the ion a net posi ve (i.e., ca on) or nega ve (anion) charge. Lithosphere
Major Cons tuents of Crust (by mass) O2 (Oxygen) | 46.40% Si (Silicon) | 28.15% Al (Aluminum) | 8.23% Fe (Iron) | 5.63% Ca (Calcium) | 4.15%
Minor Cons tuents Na, Mg, K, N, H, and others
Pedosphere
Major Cons tuents (Highly Variable) Solids | 50% Air | 25%
H2O (water) | 25%
Solids Breakdown 45% mineral par cles (inorganic) 5% organic ma er
Organic Ma er 80% Humus, 10% roots, 10% organisms
Carbon Breakdown Organic C: ~ 0.5 to 3.0 %SOC (kg Cm-2) Inorganic C: ranges from 15 to 50% of total carbon Total Inorganic Carbon = Total Carbon – Total Organic Carbon ECOSYSTEM BIOGEOCHEMISTRY
Agenda 1:40 – 1:45 | Instructor Introduction 1:45 – 2:00 | Student Introduction 2:00– 2:30| Introduction to Ecosystem Biogeochemistry 2:30– 3:00 | Syllabus Orientation