general lecture in natural environmental studies shiro tsuyuzaki, gsees, hu the abstracts of lecture...
TRANSCRIPT
General lecture in natural environmental studies
Shiro Tsuyuzaki, GSEES, HU
The abstracts of lecture will be introduced in
http://hosho.ees.hokudai.ac.jp/~tsuyu/index.html (English version),
or
http://hosho.ees.hokudai.ac.jp/~tsuyu/index-j.html (Japanese version)
Terrestrial ecosystems
Expected background
Knowing “Fundamental ecology”and/or related subjects
自然環境学総論
What lectures I have in this semester
Introduction to environmental science (intensive course)2nd class (10:30-) on Monday, Rm# C204-1One turn
General lecture in natural environment studies2nd class (10:30-) on Friday, Rm# D102Last five turns
Advanced course in watershed environmental science2nd class (10:30-) on Wednesday, Rm# C202Full (12 or more) turns
Advanced course in environmental conservation2nd class (10:30-) on Thursday, Rm #C202First six turns
Do it for me
Please do not call me ‘sensei (先生 )’.
Because my definition of ‘sensei’ = armchair scientist/professor
Tsuyuzaki Guidance (Terrestrial ecosystem and climate)Sato Solar radiation and climate Energy budget at land surface Atmospheric boundary layer and regional climate Land surface processes and climateNegishi Controlling factors of ecosystem structure Food web and material cycling Ecosystem response to environmental fluctuationsTsuyuzaki Photosynthesis and primary production Estimation of primary production Ecosystem responses to global warming Fundamental concept of modeling on temporal ecosystem changes
Syllabus
Biome (introduction)How to measure (fine-scale)
Biomass estimation - AllometryHow to measure (global-scale)
Remote sensing and geographical information systemResults
Plant growthPrimary productionBiogeochemical cycle
Field experiments and controversial ProblemsPseudo-alpine zoneNot only CO2 … but also methane(Skislope vegetation)
Warming experimentsGlobal-warming models
Content (of my turn)
Human disturbances
Scale Example
Large Global warming (+ Ozone hole) (Environmental hormone)Desertification DeforestationAcidic rain Forest ecosystem changeHeat island Urban ecosystem changeForest cutting (including skislope construction)GrazingTrampling
Small Clipping
Occurring with various scales = “Biological invasion”
Grazing,Coppice,Slush-and-burn agriculture,and others
pH < 5.6SOx, NOx brown forest soil
Ecosystem or biosysteman ecological system that includes all the organisms and their environment within which they occur naturally.
+ Plant community+ Animal community+ Environment
= Ecosystem
If you think protecting species is hard, just wait until we try to protect whole ecosystems.
Noss (1996)
Fig. 9.11. Movements of nutrients from a stream to fish, bears, and eagles; nutrients are then deposited in the uplands and absorbed into the terrestrial biota. (Turner et al. 2001)
Terrestrial ecosystem
Mountainous ecosystem
Stream ecosystem
Oceanic ecosystem
Landscape unit
Biome (formation)
a major regional ecological community of organisms usually defined by the botanical habitat in which they occur and determined by interaction of the substrate, climate, fauna, and flora.
Examples Tundra Taiga Summergreen forest Grassland Desert Tropical rain forest
(Clements 1916, Clements & Shelford 1932)
Figure 28.16 Temperature and rainfall determine the biome to a large extent. For example, rain forests are found in tropical regions where temperatures are warm and rainfall plentiful year round. Deserts, on the other hand, are found in tropical and temperate regions where rainfall is minimal. (Mader 1985)
Biome along the gradients of temperature and precipitation
Dec
reas
ing
tem
pera
ture
→
Increasing dryness →
Tropical
Temperate
Subarctic
Arctic
taiga
tundra
forestgrassland
semidesertdesert
semidesertdesertsavanna
rain forestseasonal forest
ForestsBoreal forestTemperate forestTropical forest
Precipitation = highTemperature = various
Net primary productivity = highBiomass = high
Coniferous forestA coniferous forest encircles the globe in the northern temperate zone.
Water works for gold mine
One year after a forest fire
Photo taken in Boston Creek near Fairbanks, AK, on May, 2005 (by ST)
GrasslandsPrimary regions:
Rainfall is intermediatebetween that of deserts and forests
Productivity = highBiomass = low
Savannah (Africa)Steppe (eastern Europe and Asia)Prairie (north America)Pampas (south America)
Desertification
Deserts, Semi-desert and shrubland
So-called arid regions
Precipitation = extremely lowTemperature
hot dayscold nights
Productivity depends on rainfall
TundraVegetation and animal life on the tundra. Notice that the lack of trees, which are unable to root successfully, because the ground is always frozen beneath the surface.
Sept. 29, 2006 (Asahi Newspaper)
植生調査は 10 四方ごと。パルサに生える植物の種類とその㌢割合を調べる =米国立北極行き野生生物保護区で、山本壮一郎撮影
アラスカ
植生多様なツンドラ
北大
温暖化の影響把握へ
米アラスカ州に広がる米国立北極域野生生物保護区のツンド
ラ平原にこの夏、
北海道大の環境調査隊が入っ
た。
ツン
ドラの植生の変化を人工衛星などで監視し、
地球温暖化の影響を
いち早く検地するのが狙いだ。
(
ワシントン=
上田俊秀
)
Primary regionsArctic tundraAlpine tundra
Temperature = lowPrecipitation = low
(< 250 mm), mainly as snow
Productivity = lowBiomass = lowSpecies richness = high
+ consider “Permafrost”
Fig. Schematic illustration of species richness-area curves in two different habitats (A and B).
Area
Sp
ecie
s ri
chn
ess
Habitat A
Habitat Be.g, tundra
Productivity Carbon fluxBiomass Carbon sink/source
Diversity in tundra
Scale-dependent diversity
(Raunkiaer 1934)
Avoid stressful periods (cool/hot temperature, or drought) by dormant organs
Position of dormancy budP: Phanerophytes MM: Macrophanerophytes > 8 m in height Trees M: Mesophanerophytes = 2-8 m + Epiphytes + SclerophytesN: Nanophanerophytes = 30 cm – 2 m ShrubsCh: Chamaephytes < 30 cmH: Hemicryptophytes Ground surface PerennialsG: Geophytes UndergroundHH: Helophytes UnderwaterTh: Therophytes Producing seeds Annuals
Raunkiaer’s life form or dormancy form spectra
Raunkier’s classification of life forms
(a) Trees, shrubs Warm, moist(b) Perennials Cool, dry(c) Perennials Cold, moist(d) Perennials Cold, moist(e) Annuals Deserts and grasslands(f) Epiphytes Warm, humid
Raunkiaer’s life form spectrum in the world
Ph Ch H G/HH Th
World standard 46 9 26 6 13
Tropical 61 6 12 5 16Desert 10 17 20 6 46Mediterranean 12 6 29 11 42Warm temperate 8 6 50 18 19Arctic 1 22 66 15 2Alpine - 25 68 4 4
Mean annual temperature (Co)
An
nu
al p
reci
pit
atio
n (
mm
)Summary Determinants on distribution of biome = Global scale
Temperature vs Water (precipitation)
AnnualsShrubs
Trees
Perennials
Figure 1. The distribution of traditionally defined biomes in terms of annual temperature and precipitation. The shaded area includes all biomes that contain trees. (Modified from Woodward & Lomas 2004)
Fig. 2. Net energy balance of a species along a geographical gradient, showing the thresholds for reproduction and survival (Keddy 2001)
Environmental condition
Org
anis
m p
erfo
rman
ce(K
cal/
orga
nis
m)
Growth range
Potential geographical range
Energetic costs of competitionOnly the green region will support reproducing populations. By increasing the costs of survival, that is, decreasing the net energy balance, competition reduces performance and narrows distributional ranges.
Reproductive range