Fog in the California Redwood forest: Ecosystem inputs and use by plants T.E. Dawson.

Slides:



Advertisements
Similar presentations
The effects of large deforestation (in the Amazon)
Advertisements

Oxygen and Hydrogen in Plants. Outline: Environmental factors Fractionation associated with uptake of water Metabolic Fractionation C3, CAM and C4 plants.
C4 has two features that are advantages in warm, dry
TROPICAL RAINFOREST PAGE OBJECTIVES Describe and explain distribution of tropical rainforest. Describe the features of tropical rainforests. Describe.
Tropical rainforest models
Nitrogen Isotopes in Animals: Systematics Timothy Lambert (adapted from 2007 presenter) Earth 229, Winter 2010
Structure and Function
ECOLOGY AND THE BIOSPHERE
Hydraulic redistribution in Amazonian trees Rafael S. Oliveira 1, Todd E. Dawson 1, Stephen S. Burgess 1,2 Daniel C. Nepstad 3 1 University of California,
Plant Adaptations.
 Constant warmth and rainfall provides the home to most of the species on Earth.  > 70% of all terrestrial species  Question:  How does the structure.
Topic 6 in Review Book.  global wind patterns  ocean currents  the water cycle.
Water Isotopes in the Hydrosphere I10/10/05 Lecture outline: 1)the hydrological cycle  D and  18 O variability 3)fractionation processes  18 O,
Redwoods go wireless: discovering the links between trees and the hydrological cycle Todd Dawson Center for Stable Isotope Biogeochemistry & Department.
“Carbon Isotope Systematics in Soil” -or- “Plant Poo and Microbe Farts” Justin Yeakel, UCSC.
Keystone Species Coastal Redwoods Saguaro Catci Sea Birds Scott Rohlf 3/1/10.
Carbon Isotope Systematics in Soil. Soil Pathway Summary Organic matter finds it’s way into soils and decomposes SOM (Soil Organic Matter) is further.
Evaporative heat flux (Q e ) 51% of the heat input into the ocean is used for evaporation. Evaporation starts when the air over the ocean is unsaturated.
Adaptations (3) How do plants and animals survive?
Forest are ecosystems in which many trees grow..
Primary focus of studies: Tracing water uptake sources The Canopy Effect Tree-leaf Temperature Hydrogen & Oxygen in Plants: Applications Modified by Guangsheng.
3.2 Terrestrial Biomes.
CLIMATE.
U1LG3: Climates & Biomes Criteria for Success:
Climate.
World Biomes Deserts. Global Air Circulation.
DESERT BIOMES DESERT – AN AREA WHERE EVAPORATION EXCEEDS PRECIPITATION.
Plant and Animal adaptations
4 How do animals and plants survive in the Sonoran Desert, Arizona, USA ? 4 A presentation supplied by North Chadderton School, Oldham, Lancashire, England.
Canopy Forest Floor Roots. What is forest hydrology? Forest hydrology is the study of the interactions between the hydrological cycle and forest ecosystems.
Atmospheric Circulation in a nutshell Hot air rises (rains a lot) in the tropics Air cools and sinks in the subtropics (deserts) Poleward-flow is deflected.
The water cycle, also known as the hydrologic cycle or H 2 O cycle, describes the continuous movement of water on, above and below the surface of the.
Where Living Things are Found.
Climate and Terrestrial Biodiversity. Hoh Rainforest (140 – 170 inches rainfall per year)
HOW THE FOREST WORKS.  The rainforests contain 50% of all the plant and animal species in the world.  The Amazon rainforest is 30 times the size of.
Parts of a Plant. Flower  Reproductive organ of the plant  Flowers are usually both male and female  The male part of the flower is the STAMEN  The.
Unit 7: Plants 7.0 Botany: The study of plants. 7.1 Characteristics of Plants -Multicellular -Nucleus with DNA -Photosynthesis -Cell Wall -Sessile (Do.
Chapter 6: Climate and Terrestrial Biodiversity
An ecosystem is all living and nonliving things in an area.
Only rain forest located in the tropics or ten degrees within the equator have year round warm weather. Subtropical rain forest that lay outside the.
Tropics Regions between 23.5 ° N and S (tropics of Cancer and Capricorn). These are areas where the sun is directly overhead at some point during the year.
AOSC 200 Lesson 3. Fig. 3-1, p. 54 Fig. 3-3, p. 56 Diurnal temperature cycle.
ECOLOGYECOLOGY Chapter 34. Ecology- The scientific study of how organisms interact with their environment and with each other.
Climate: The average, year-after-year conditions of temperature, precipitation, winds and clouds in an area.
화양초등학교부설영재학급 조승희.  Flower most have pollen.  Birds, insects, and the wind help spread it from flower to flower.  Pollen helps plants make seeds.
Earth’s climate and how it changes
Ecology: Abiotic Factors. Ecology: Abiotic Factors Unit Concept: Everything is connected to the non-living environment.
Plant Adaptations. Co-evolution Pollinators evolved with flowers. Flowers evolved with pollinators. They are intertwined.
Earth’s Energy Budget. Modes of Energy Travel Heat Energy can be transferred in three specific ways: Heat Energy can be transferred in three specific.
“The gradual change over time in the species that form a community”
Seeds appear in fruits Seeds eventually grow into new plants.
C LIMATE Chapter 21. F ACTORS THAT A FFECT C LIMATE Latitude Less solar energy as you move away from the equator Tropical zones Rays from the sun hit.
All living things depend on Earth’s cycles to provide them with what they need to survive. These cycles produce oxygen, water and important nutrients.
Desert Tundra Taiga Forest
Chapter 4: Ecosystems & Communities Starting with … Climate (4.1)
Terrestrial Biomes Ch 6 SEV2.c: Characterize the components that define a Biome. Abiotic factors-to include precipitation, temperature and soils. Biotic.
Indianpipe –Monotropa uniflora. Tetraphis pellucida.
Biodiversity total number of species within an ecosystem and the resulting complexities of interactions among them Biomes all of the life-supporting regions.
Levels of Organization & Biomes Chapter 34. What you need to know  The levels of organization ecologists study  The role of abiotic factors in the formation.
Study of Plant Parts and Functions
Starter: When is the Earth closest to the sun?
Hydraulic Redistribution of Soil Water in a Drained Loblolly Pine Plantation: Quantifying Patterns and Controls over Soil-to-Root and Canopy-to-Atmosphere.
Temperature Variations
Tropical rainforest models
Introduction to Ecology: Historical Foundations and Developing Frontiers Chapter 1 Copyright © The McGraw-Hill Companies, Inc. Permission required for.
Climate and Terrestrial Biodiversity
CLIMATE.
Paleoclimate Proxies A proxy is a natural data set that mimics an environmental change, e.g. increased tree ring width and increased temperature and moisture.
Tek 10b describe the interactions that occur among systems that perform the functions of transport and reproduction in plants Transport Plants have special.
Translocation and Transpiration
Presentation transcript:

Fog in the California Redwood forest: Ecosystem inputs and use by plants T.E. Dawson

Objectives Is fog an important source of moisture for the plants that inhabit the ecosystem –Redwoods use 600±145 L/day (45 m tree) –Greatest demand during summer when rain is sparse, but fog is common –During summer, deep soil water may become unavailable for shallow rooted species –How much is actually used, not just stored? Areas with redwoods and without –Trees significance in influencing the magnitude of fog water input into the ecosystem

Importance of Fog Ecosystem nutrient balance or aspects of biochemistry Reduce plant moisture stress by reducing canopy transpiration or evaporation from habitat Improve plant water status by direct absorption When trees are removed water input from fog drip deceases and so does streamflow Higher water input/soil moisture around tree canopies

Fog formation Heaviest from midnight to early or mid-morning Interaction between warm air and cold water (up-welling, or currents) Causes condensation---thus fog Doesn’t require condensation nuclei like clouds Enriched in the heavier 2 H and 18 O isotopes relative to water source (ocean) Heavier then rain because rains come from storm systems that have moved great distances, which causes them to become depleted in 2 H and 18 O

Methods Fog and rain samples –Total input Rain, fog, fog drip off trees –Local meteoric water line  2 H=7.7  18 O+9.6 Provided a mixing line that was more useful for interpretation local variations Plant and soil samples Plant water use –Whole tree transpiration –Sapflow sensors Different size trees

Mixing Models Proportion of fog water (P f ) used by plants –Two compartment mixing model (Brunel et al) Assumes water comes from 2 sources –Fog and rain –Deep soil/groundwater Weighted values-not all sources are equally available

Results Interception off trees always higher by 18-40% -stripping fog -solar radiation, wind velocities Forested areas have greater input

Redwoods: 8-43% Understory: 6-100% Rooting patterns, water demand, direct absorption through leaves, funnel water

Water use patterns Fraction of fog within xylem that was used 13-45% of all water used annually –Smaller trees used more Obtain ~19% from fog –Water use is higher in summer when trees take up and use more fog water –More important source than isotopic information implies

El niño: ratio of rainfall to fog water input higher (less fog), Pf and coefficient of variation increased -plant demand for water was highest in summer when there was no rain, and fog inputs did occur Dry: Less rain in winter, so more dependence on fog in summer

VS. Intact forests increase annual income of water -if moisture inputs decline, so do nutrient inputs, decomposition and mineral cycling -therefore, tree loss = more drought prone, warmer, open ecosystem -plants will experience more water stress

Saguaro Cactus : How important are they? (Wolf and Martinez del Rio)

Saguaro cactus Succulent CAM 4000 or more liters of water 300 flowers, 50-60% fruit A ton of pollen, nectar, fruit—to attract pollinators and seed dispersers Produce fruit during driest months (June-July) Fruit : water and sugar Seeds: protein, lipids and carbs  13 C = -13.1±0.2 ‰ –Most common C3= ±0.2 ‰  D = 48.4±1.6 ‰ –Surface water=-37.3 to -23.5‰

Desert Nesting Birds Mourning Dove Gained only nutrients (35% total C) for ~3 weeks in July No correlation between  13 C and  D White-winged Dove Saguaro fruit = >60% of diet between June and mid-Sep.  13 C and  D linearly and positively correlated—fruit was important for C and H 2 O Differences in foraging modes!!

Importance for community of Sonoran Desert birds… Determining proportion of diet that is represented by two isotopic sources: isotopic composition of 2 sources –  tissue = p(  1 +  ) + (1-p)(  2 +  ) Isotopic discrimination factor(  tissue -  diet ) fraction of diet incorporated into focal tissue Blood plasma –Stable C3 resource signal in bird plasma during periods when they saguaro fruit was not available –Thus-  = +3.3‰ –Reflects isotopic composition of C incorporated recently

 13 C of plasma during summer showed distinct swell—coresponds to Saguaro input into ecosystem without:  13 C= -21.6‰ with:  13 C= -16‰ 43% of avian community’s carbon derived from fruit Lasted for ~ 6 weeks

Individual species Granivorous and frugivorous Insectivorous (7 of 16 that get 25% diet from cactus)

Deuterium  D of fruit water is enriched ‰ White-winged Doves –When using fruit, body water pools became enriched –Strong correlation between C and D Body water discrimination factor –Enriched above fruit Evaporation But…the presence or absence of a correlation between  13 C and  D can be used to determine whether birds feed on seeds, or pulp as well