Geography 40
Global Environmental Change
Fall 2002



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Lecture28: Tropical Ecosytems

Tropical biodiversity

Introduction to tropics


Definition—depends on who is defining, that is biologists often use specific plant assemblages, climatolgists may use specific atmos. conditions, geomorphologists may rely on specific physical processes.

Koeppen
In General, the tropics as falling within the 23.5N and 23. 5S. This latitudinal boundary defines the range of the subsolar point and this area therefore receives large amounts of solar radiation throughout the year, with little annual fluctuation.
brazil
This is reflected in climate graphs that show rainfall and T which are typical for the tropics.
Compare with SF

Classification:

lushforest paramo
PHOTO REMOVED PER REQUEST OF COPYRIGHT HOLDER
sahel
There are a variety of environments found in the tropics; humid, subhumid, dry, alpine, montane, etc. One way of looking at the different tropical climates is the Koeppen classification system.

Koeppen
You can look at this more closely in the Christopherson textbook. To define a tropical climate, it uses a mean T of 18ºC for the coldest month, which excludes the cooler highlands. Like I said, we often think of the tropics as the humid lush environment of the tropical lowlands but around 25% of land surface within the tropics is considered highland, above 900m. As you can see, these classifications divide the tropics up into many subcatagories. There are many other classification systems and they very rarely fall out along the same boundaries. It is important to remember that whatever system of classification used, the categories at best describe transition zones both within the tropics and the tropics themselves.

rainfall
Precipitation: As a result of the stability in annual T, differences in precipitation are much more important than annual T as a climatic parameter. Most tropical rainfall is associated with convective processes rather than frontal systems. Remember that the ITCZ is basically composed of convective cells rising; convective uplift can occur away from the ITCZ simply because of the heat created by the high solar input.
The annual migration of the ITCZ is an important factor in creating seasonality of rainfall that we see in the tropics. Areas closer to the equator experience less seasonality; those at higher latitudes tend to have more pronounced seasonality.
Seasonality in the tropics refers to wet and dry as opposed to cold and warm. This is most obvious when looking at deciduousness in the tropics. Deciduous trees that we are familiar with in the temperate areas lose their leaves as an adaptation to cold winter months, deciduousness in the tropics is an adaptation to get through dryer times of the year (to not lose water through respiration). In general, rainfall varies dramatically throughout the tropics and has a strong influence on the ground in the form of species composition, diversity, and growth rates etc.
A good example of this is the Yucatan peninsula, which has a pretty steep rainfall gradient over the latitudinal distance of 5º, with rainfall dropping from around 2500mm/year in the south to around 1500mm/year in the north. This is reflected on the ground: where forest still exists in the south, it is high, closed canopy, broad leaf luxuriant forest. In the north, the forest is comprised of much smaller trees, basically thorn scrub.

Neo/Paleo: A quick point, that the tropics are often divided into two groups, along the lines of the old world/new world divide. That is the Americas being the new world, and the tropical areas of the Americas are referred to as the Neotropics


Diversity in the tropics

Measuring diversity and theories of tropical biodiversity.

butterflies
Diversity increases as one gets closer to the equator. Here is one image that shows, for example, that shows a common biogeographic pattern—the decrease away from the equator in number of swallowtail butterfly species.

Measuring diversity by species richness: the total number of species found in a given area.
Simpson’s Diversity Index: looks at the likelihood of two sampled individuals being the same species.

species/area

Another important way of measuring at diversity in the tropics is the species-area curves. Species-Area curves show the number of species found as the unit area increases. Big difference between the tropics and temperate latitudes is that in the tropics, these curves tend to not level off because there are so many rare species.
Thus, tropical diversity tends to be associated with a lot of rare types and a few common ones. For example, a 50ha plot in Panama with about 240,000 stems counted showed 309 species. 50% of the species had fewer than 110 individuals (17000). Again, any way it is measured, diversity increases toward the equator.

Theories of biodiversity: Why is there so much diversity in the tropics?? This has been the topic of much debate, and many theories have been put forth.

I. Interspecific Competition Hypothesis:

Also known as niche partitioning. Basic idea is that 2 or more species seeking access to the same limited resource must subdivide the resource, or one will win over the other. The idea here is that if a resource is not subdivided, a species that is better adapted will eventually out-compete other species.
partitioning
This theory argues that high levels of competition in the tropics have led to increased specialization, which allows for greater packing of species into a smaller area.

Finchbillsfinchetree
This high level of specialization definitely exists and is an interesting component of the tropics—one of the best examples of this is the finch population in the Galapagos. These finch poplulations were first described by Charles Darwin in the 1830’s and were important to his developing theory of natural selection. Basically on this island chain, there is a high diversity of finches with small differences in beak morphology. These differences in beak morphology reflect different feeding methods, which allow these species to co-exist without competing for food.
This process that leads to this is known as adaptive radiation. Basically, a single species may, over time, branch out to form many species, each with a specialized adaptation for a specific resource.

fruitbatinsect (Looks like another fruit bat to this web technician)
Bats are another good example. There is generally an amazing array of bat diversity in the tropics. (fruit, insect)The high number of bat species falls out along food procurement strategies; in any given area you can find bats that eat meat, fruit, fish, blood, nectar, and insects. Insects can be eaten from all over the place as well.

Problems:
Plant Species don’t compete: There is very high plant diversity, but most trees compete for the same resources—space, light, moisture and nutrients. While there are some specialists, most trees are resource generalists and only differ along a small gradient of required resources.
Not specific to the tropics
There are people who are still looking at this theory. In the end, the argument is circular if one argues high level of competition results from and leads to many species that are after the same resource.

II. Predation Hypothesis:
Predators prevent prey species from competing with each other to the point of extinction. Predators will constantly switch their attention to the most abundant prey. Example of four caterpillar species—one wins out, but the birds begin preying more on the populous species, limiting it and allowing the others to survive. This is called density-dependence in plants and frequency-dependence in animals, meaning that the degree to which a prey will be selected is dependent on its density (if plant) or frequency (if animal).

So in a mixture of species, as one species becomes more common, mortality increases, limiting that population and preventing it from out-competing other species.
Note that this is essentially the opposite of the Interspecific Competition Hypothesis. Rather than specialization developing, predators would essentially prevent it by keeping competition levels low.
Problems:
Some studies have shown that large cats for example do not selectively choose the most populous food source, but eat everything they find. This would accelerate the extinction of those species that are already loosing out to competition
Also not clear why this is limited to the tropics.
So this is a strong theory, but evidence supports it shows an importance in structuring plant communities. However, it is a mechanism for diversity maintenance and does not address origin of diversity.


III. Productivity/Resource Complexity Hypothesis:
The tropics have more productivity (biomass) which allows more species to be accommodated. Abundance of resources can lead to specialization and increased diversity. Basically this is saying that rather than competition driving species to adapt, the availability of resources is so great that species will drift toward specialization and therefore increase diversity.

lushforest
Tropical forests are structurally very complex, and this often does permit greater species packing. Resource complexity also includes disturbances such as storm damage, landslides, and tree fall gaps.
Tree fall gaps provide a patch of bright sunlight on what would otherwise be a dark forest floor. People are beginning to think of tropical forests as essentially shifting mosaics of small disturbances in recovery. Specialization for light gaps, dark under-story etc is a response to the heterogeneous environment, which leads to high species diversity.

interdist
Intermediate Disturbance Hypothesis, which falls under Resource Complexity. Intermediate refers to both the frequency and the scale of the disturbances.
Disturbances occur at different time scales and intensity. Too frequent results in low diversity because only those species with an ability to quickly colonize will have time to do so. As frequency slows down, more species (those with lower dispersal/growth) are allowed time to colonize. If the frequency is too slow, there is time for competitive advantages to eliminate species and decrease diversity.

Medium intensity disturbances also lead to higher diversity. Too small means only the nearest species will most likely colonize. Too large means that only species with high dispersal ranges can colonize. A medium size, with some species left alive, allows for the broadest range of potential colonizers. The tropics have a lot of rainforests of mixed age and composition, which supports this idea.
Problem:
Structural diversity does not correlate with species diversity.
For example, there is no correlation between forest complexity and bird diversity in the tropics.
It is not clear that the tropics are different than the temperate zone in regards to disturbance, seasonality.
Also there is evidence that the patchy species distributions associated with forest gaps are transient and the resultant forest composition and diversity is similar to the rest of the forest.
High productivity is probably essential to support the diversity of life forms, but not really a driving force
This is a good hypothesis—but again, it does not stand alone. It does shed light on how tropical ecosystems work.

IV. Stability-time Hypotheses.


The tropics have been stable over a range of time scales. Seasonal variation is low; so is variation of solar insolation. Much of the tropics are geologically old, they are the cratons of old crustal material, heavily eroded because of the high amounts of precipitation. Glacial erosion is nonexistent in the tropical lowlands and for a long time people thought that there was little or no T change during glacial periods.
This stability has provided the opportunity for high speciation and low extinction rates, leading to high diversity.
This theory runs contrary to the Intermediate Disturbance Hypothesis.
Problems:
Would allow for development of diversity, but not drive it.
Big problem—the tropics have not been climatically stable. The Pleistocene glaciations had an effect on tropical climates. We know from isotope and pollen studies that during glacial periods parts of central America and the Amazon basin were 4-6ºC cooler than today, CO2 was much lower, and there is strong evidence that much of Africa was drier.

V. Refugia Hypothesis

As the evidence for climatic instability in the tropics began to surface, a new theory developed based on unstable conditions, the Refugia Hypothesis:
So this theory is a response to the evidence against the time/stability hypothesis.

refugia

This theory states that during glacial periods, precipitation dropped so much in S America, that the Amazonian rainforest was broken up into smaller refugia, surrounded by vast areas of grassland.
The shrinking and fragmenting of the forests resulted in geographic isolation, islands essentially, surrounded by seas of grassland. The populations on these rainforest islands would then speciate, creating new species.
Once the glacial dryness ceased, the rainforest pockets would expand, the result being more overall diversity.
This theory was put forth in the 1960’s based on the presence of centers of extremely high diversity, which tend to correlate today with areas of higher rainfall. The idea is that in the past these areas may have had higher rainfall, which could have supported the rainforests.

This hypothesis has been the center of much debate, with much focus on the degree of environmental change in the tropics during the glacial period.
One problem arises from the lack of evidence—lakes that hold good records are few and far between in the Amazon. Some records do exist however, and the evidence disputes the refugia hypothesis.

pollen
Paul Colinvaux had produced a couple of records using proxy data (primarily pollen data) to show that Amazonian rainforests stayed more or less intact during glacial periods.
These pollen diagrams are by no means conclusive however, and this remains one of the largest debates in tropical paleoenvironments.


Conclusion:

The Interspecific Competition, Predatory and Time Stability Hypothesis are all based on the idea of equilibrium in the tropics over long time periods. More recent understanding of both long term (glacial/interglacial) and short term (treefall gaps) instability have led to new ideas about the development of tropical biodiversity. Understanding the forces behind tropical diversity is important when one considers the large scale environmental changes that are being created by human activities such as logging and burning fossil fuels.

Lecture 29: GUEST LECTURER: Madeline Solomon on
Social and Human issues and ecology of the Tropics

Background:
Tropics lie in band from 23.5N and 23.5 S latitude.
35% of Earth surface is covered by the Tropics
7% of Earth surface covered by tropical forests, but
53% of total world forestland is tropical forest
Little seasonal variation in Temperature, but considerable variation in precipitation
1/2 the world’s population lives in the Tropics, or about 3.5 B people
800 m of them are malnourished
food production must double to feed all of the population, which leads to increased stress on the land
Tropical forests are one of the most productive ecosystems on Earth.
Types of tropical forest:
Wet – no distinct dry season
Moist – short dry season (s)
Dry (seasonal) – pronounced dry season, forests are deciduous
Montane – forests at higher elevation
Cloud – forest at highest elevation, with fog. Many endemic (locally restricted) species.

Ecological Characteristics
Structural complexity
Biodiversity is very high
Dynamic system – disturbance is common
High productivity and nutrient cycling
Phenology – seasonal timing of life history events (flower at different times of year)
Specific pollinators
Drought sensitive
Fragmentation due to deforestation
Ecosystem Services – attempt to quantify why we should save the forests
Regulate climate
Maintain soil moisture
Reduce sunlight penetration
Limit soil erosion
Maintain diversity
Provide habitat and resources

Carbon Cycle
In tropics the carbon (C) stored in the biomass is equal to the C stored in soil
Whereas in the temperate regions, C in biomass is much less than C in soils
Rapid carbon processing (and nutrient processing)
Therefore, High Productivity, rivals wetlands
Measured by 1) measuring the Net Primary Productivity (NPP): NPP = Photosynthesis – Respiration (litterfall is usually used as a proxy); 2) REMOTE SENSING
Mature tropical forests are in near equilibrium with the atmosphere, while overall, terrestrial biota is a C sink.
Deforestation changes this C balance by:
Increasing C source to atmosphere
Increases decomposition at the surface (puts C into atmosphere)
Increases evapotranspiration due to warmer soil surface
Decrease in woody component of the forest, which stores C long term

Land Use Change
Really means Deforestation.
Spectrum of deforestation: from temporary small clearing ------‡ major clear-cutting
Small scale operations by subsistence farmers has relatively low impact
Causes for Deforestation:
Conversion of land to agricultural use
Logging
Shifting cultivation (slash/burn) – often low impact, except when increased population pressure drives more people to this form of agriculture
Infrastructure (road building)
Charcoal production
Over exploitation
Fire (natural and human-caused) – more deforestation -> more fragmentation -> more edges which are drier -> more fires
The primary causes for deforestation differ between countries.

Impacts of larger-scale Deforestation:
No trees, or damaged trees
Decreased productivity
Increased CO2 emissions
Increased erosion
Forest regeneration is inhibited
Short-term floods
Overall reduced evapotranspiration -> less water into atmosphere -> less convection -> less precipitation
Increased surface albedo – localized cooling of the land and therefore less evapotranspiration

Global Climate Change
Greenhouse effect – keeps Earth’s temperature at around 14 degrees C, livable
Natural Greenhouse gases, water vapor, CO2, CH4 (methane), N2O, others

Biosphere-Atmosphere links and feedbacks
Feedbacks:

Water --+--Earth Temp --+-- Greenhouse Gases--+ -- Greenhouse Effect --+ --Earth Temp.
Add Deforestation:
Water -- – --Deforestation --+ -- Greenhouse Gases.

Climate Projections: 1.4 – 5.8 °C increase by 2200. Global Average looking at Best guesses.
Likely effects:
Higher elevation ecosystems – haven’t any higher ground to move to – e.g., Cloud forests and alpine forests are at risk.
Precipitation variability will increase – both droughts and severe storms
Debate about land use change – how it fits in with Global Change:
People increase Greenhouse gases
Oceans’ inertia causes temperature changes to be slow and long term.

Lecture 30: Short-term variability cont’d: El Nino-Southern Oscillation

Present-Day Climate Variability - El Nino
READING: Ruddiman, "BOX 16-2 Climate Interactions and Feedbacks". On Reserve.
Quiz – Next Friday. Covers from Holocene variability to today’s lecture on El Nino.

November 7, 2002 — Climate and weather experts from NOAA today said El Niño remains on track to influence weather across the United States during the upcoming winter season. Currently, NOAA scientists classify the El Niño’s intensity as moderate, but are watching closely for any further strengthening. "Following the recent trends, we expect the waters in the eastern equatorial Pacific to continue to warm, and mature El Niño conditions will prevail through February 2003. Although an increase in the strength of this El Niño is possible, we don’t expect it to compare with the 1997-98 version. Also, the global impacts should generally be weaker" said Vernon Kousky, a meteorologist at the NOAA Climate Prediction Center.

What it is:
The name El Nino used to refer to the warm ocean current that flows along the coasts of Peru and Ecuador for a few weeks each year around Christmas. Local fishermen named it El Nino after Christ. Now the name is used to describe a major shift in oceanic circulation that occurs in this region of the Eastern pacific every 2 to 7 years on average.
During an El Nino event, the normally cold surface water temperatures off this part of the So American coast are warmed by upwards of 5 degrees C.
This warming of the surface waters in this region results in plankton population crashes, which in turn cause fish, mammal and bird populations to decline. In addition, the warming of the surface waters causes increased evaporation off the water, which then causes extreme rainfall over the land, and this area along the coast is desert (littoral desert), so there are often flash floods.
But while the changes in ocean and atmospheric circulation occur in the tropical Pacific, the effects of El Nino are felt outside the tropics as well.

What causes:
Fundamentals of Equatorial Atmospheric Circulation
Normal conditions: during a normal year, the waters off the coast of So. America are fairly cool: around 18 degrees C compared to typical tropical ocean surface water (25 degrees C). This cooler water is due to upwelling off the coast, bringing lots of nutrients which feed the plankton, and forms the basis of an important food web. These waters are very productive.
Non-El Nino yearEl Nino year

Atmospheric Pressure
To understand why the coastal current here is cold and this is a zone of upwelling, we have to go back to Atmospheric circulation patterns.
Superimposed upon the Hadley circulation cell (remember, a primarily North - South circulation) is an important East - West circulation pattern in the troposphere over the equatorial Pacific ocean. The Pacific ocean is the largest ocean basin, which accounts for the strong development of this E-W circulation, though smaller cells of convection form over Eastern So. America and Africa.
The region of the Western equatorial Pacific has the highest sea surface temperatures in the world. This region includes Australia and Indonesia, and because of the high sea surface temperatures, it is an area with intense atmospheric convection.
Some of the rising air moves Eastward across the Pacific, subsiding over the middle of the Pacific, but also further east, off the west coast of So. America.
The circulation is completed by air flowing at the surface to the West.

The East West circulation produces an oscillation in the sea level pressure distribution between the western and the central/eastern part of the tropical Pacific called the Southern Oscillation. When pressures are low in the west, they tend to be higher in the east, and vice versa.

Ocean circulation
The persistent easterly wind (from east to west) over the Equatorial Pacific causes water to pile up in the western part of the basin. Warm water therefore accumulates in the western Pacific, on the order of a meter or so. The relatively thin layer of surface layer on the East side allows for upwelling to occur, bringing up the nutrient rich waters and promoting high biological productivity.
This is the "normal" pattern.
But, every few years this pattern breaks down and an "El Nino – So. Oscillation" (ENSO) event occurs.

El Nino Conditions
It is still unclear exactly what causes an El Nino.
Remember, convection in the western pacific occurs because the water temperatures at the surface are so high, but the sea surface temperatures are high because of the atmospheric circulation, which is driven by convection.
This is a single, integrated system, and perturbations at any point will cause changes throughout the all the components.
During an El Nino, the strength of the Easterly surface winds drops, or even reverses direction. This affects the pile up of warm water in the western Pacific, as there is nothing holding the piled up water there and that water then comes sloshing back across the ocean in a Kelvin Wave, taking about 60 days to travel across the Pacific.
This shifts the pool of warm surface water to the Central Pacific, which then changes the atmospheric circulation pattern.
It also shuts off upwelling in the eastern Pacific.

Convection shifts towards the central Pacific, which shifts the East West Circulation.
Climate impacts include severe drought over Indonesia and Australia, and drought also in central America, Brazil and southeast Africa.
Flooding and high rainfall occurs in the central pacific, and on the west coast of So. America, in particular on the dry slopes of the Andes in Ecuador and Peru. These cause landslides and high erosion.
ENSO also appears to affect the monsoon circulation over India, causing increased rain over southern India and drier conditions over northern India and the Himalayas.

Effects – duration 1 to 2 years

Regional
Outside the tropics, El Nino events tend to be different each time. For example, over the western U.S. the El Nino year 1976 was a serious drought, while 1982 was a very wet year.

Next time – how El Nino affects Coral growth in the tropical oceans.

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