Freshwater Riches of the Amazon
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Size is at best a partial explanation for the Amazons bounty. |
A second general pattern, which holds true for tropical Americas birds, reptiles, amphibians, mammals, insects, marine fishes, invertebrates, and plantsthat is, most organismsis known as the latitudinal diversity gradient. Long recognized but never fully explained, this is the trend for life to be more diverse in tropical, low-latitude regions. It is a fact of geography that near the equator, the earth receives more energy from the sun. Temperature and day length are more seasonally stable (although in many cases rainfall is not). Under these conditions, vegetation abounds and, in turn, can support many animals of many species, including some that have extremely specialized lifestyles and exist only in small populations. The Amazon is full of gastronomic specialists. Hypophthalmus, for example, eats tiny zooplankton; other fish eat snails (Megalodoras uranoscopus), the scales of other fish (Catoprion), the tails of other fish (Magosternarchus), chunks of flesh and fins (piranhas), fruits and seeds (tambaqui), wood (Panaque), or blood and gills (candirú catfish). (One species of candirú catfish, which is attracted to the flow of water from the gills of its prey, has become notorious for its unfortunate tendency to mistake a stream of urine for gill flow and to enter human urethras.)
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While heat, sunlight, and ample food can help maintain tropical diversity, they do not explain how great diversity arose in the first place. The bounty of the Amazon can be accounted for only if we consider time as well as space. Biogeographical patterns, particularly those of fishes, are rooted deep in the past. As denizens of rivers, streams, and lakes, the largest groups of endemic, or native, freshwater fishes in South America are relatively confined. Unlike many other creatures, they can neither move through coastal saltwater nor traverse land barriers. Where they are and how they move about depend on changes of continental proportions that have taken place at a geologically slow pace.
One controversial theory that seeks to explain tropical Americas biodiversity holds that climatic shifts starting about 2 million years ago and continuing through the Pleistocene Epoch, or until about ten thousand years ago, caused the repeated fragmentation and merging of tropical rainforests. Such shifts provided multiple opportunities for birds, butterflies, and plants to diverge and eventually become new species. But in the case of fishes, a time frame of 2 million years is just yesterday. Long before the Pleistocene, the Amazon teemed with species that are closely related to fishes alive today in the river.
![]() For fishes, 2 million years ago is just yesterday. |
As early as the middle Miocene, about 15 million years ago, the tropical American fish fauna was essentially like todays. It included many living groups: stingrays, lungfish, pirarucú, piranha, goliath catfishes, some electric fishes, and cichlids. A primatologist friend and colleague once showed me a fossil of a 13-million-year-old fish he had excavated in Colombia. He had no idea what kind of fish he had found and was struck by its particularly large teeth. He was surprised when I was able to identify the fossil; the specimen looked just like a living fish I knew well, the tambaqui. Although no longer found in the rivers of central Colombia, the tambaqui, which feeds on seeds and fruits that fall from trees in the seasonally flooded forests, thrives today in the Amazon. Similarities between ancient and modern fishes crop up even further back in time. One well-preserved fossil fish about 59 million years old looks like, and is indeed related to, the Corydoras catfish popular today in the aquarium trade. And some fossil catfishes, lungfishes, and characins date back to the Late Cretaceous, 70 million years ago.
Today, 93 percent of South American freshwater drains into the Atlantic, but this was not always the case. The stage on which the present pattern of rivers took shape was the continent itself. The players, South Americas major physical features, included two huge slabs of stable continental crust, known as the Guyana and Brazilian Shields; the dynamic Andes mountain range; and the vast lowlands that lay between the shields and the mountains. About 90 million years ago, South America and Africa (both of which had earlier been part of the southern supercontinent of Gondwana) separated from each other. As South America, which comprised a continental plate, moved west, it crashed against an oceanic plate moving east. The collision caused the land along the west coast of South America to rise up, and the first stage of Andean mountain building began. During their long history, the Andes underwent several phases of uplift and subsidence. As the mountains grew, adjacent land to the east and north buckled, forming a troughlike basin running north and south. At times the basin was filled with sediment; at wetter intervals it contained large lakes, was periodically inundated by shallow ocean waters, and channeled major rivers in a northsouth direction. Taken together, the formation of Andean and other land barriers, the shifting courses of rivers, and sporadic incursions of ocean waters would have produced many opportunities for fish species to evolve as some populations were isolated from others and began to adapt to new conditions.
Long before the end of the Miocene, a great river, consisting of what are today the western Amazon and the Orinoco, flowed north through the lowland basin and into the Caribbean. About 10 million years ago, the rise of the eastern Andes created the Magdalena River basin in Colombia. Uplift continued until, by 8 million years ago, the mouth of the north-flowing Amazon-Orinoco was dammed. The river could no longer reach the Caribbean Sea. This major event in the geographical history of South America split the Orinoco and Amazon and reoriented their course from northsouth to westeast. The Amazon began to flow into the Atlantic, as it does today. Over time, new rivers appeared in the north, and 3.5 million years ago the elevation of the Isthmus of Panama formed a bridge between the American continents.
As rivers appeared, disappeared, and changed course, their communities of fishes went along for the ride. The ranges of various species expanded, merged, or were disrupted. The geological upheavals that divided rivers and river basins provided opportunities for speciation when fish populations were isolated. The results are the species that today are found only in those systems. However, fossils from the regions now occupied by the Magdalena River and Lake Maracaibo show they once contained fishes no longer found there but that still inhabit the Amazon. These include lungfish, Arapaima, tambaqui, piranha, Hydrolycus, and goliath and pirarara catfishes. Although the fossil record documents such localized extinctions of living fish groups, we have no evidence of widespread extinctions and only two or three cases in the past 65 million years in which an Amazon fish species was completely extinguished.
The biodiversity equation is balanced by speciation on one side and extinction on the other. Low extinction rates are part of the formula for fish-species richness in the Amazon basin and eastern South America. But in other regions of the world, freshwater fishes also provide textbook examples of rapid species formation. Chief among these examples are the African cichlids, which, in a geologically brief period (perhaps less than 100,000 years), evolved into hundreds of species that now live in the same body of water. In contrast, we have no evidence for any unusually high rates of speciation among fishes in South America. Given enough time and low extinction rates, a normal tempo of speciation gave rise to the Amazons array.
Since the day I recognized my colleagues fossil as almost identical to a modern fish, I have discovered several other examples of this phenomenon, and I am still struck by the great antiquity of many of the living tropical American fish species. By comparison, the history of other groups, such as mammals, has been fast paced and marked by high turnover. Tropical American mammal species have immigrated, emigrated, evolved, and gone extinct with a rapidity that makes Amazon fishes look frozen in time. Fish like the tambaquiwhose fossil and modern jaws and teeth reveal unmistakable similaritieshave, except in the restless edges of their ranges, changed little over the past 15 million years. As continents separated and connected, as the Andes grew and rivers took right-angle turns, the tambaqui persisted in its specialized diet of fruits and seeds. This fish and many modern-day finned icons of the Amazon recount a long and enlightening chapter of the story of life on earth.
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Ichthyologist John Lundberg began studying the fishes of South America’s Orinoco River in 1974 and those of the Amazon River in 1990. His pioneering surveys of the fish life of deep river channels have turned up many new species, including catfishes and electric fishes with unusual lifestyles. Lundberg, left, says his innate attraction to fossils has led him to broaden his focus; he uses insights from paleontology, geology, and biogeography in his work on tropical fish diversity. Formerly a professor at Duke University and the University of Arizona, Lundberg is now curator of ichthyology at the Academy of Natural Sciences in Philadelphia and holds adjunct professorships at the University of Pennsylvania and Drexel University.
After an autumn 1997 trip down the Amazon with a boatful of friends and scientists, artist Ray Troll was inspired to produce his most ambitious work to date: a mural-sized canvas that took a year to complete and that portrays about 120 speciesfurred, feathered, but mostly finned. Troll lives in Ketchikan, Alaska, but travels frequently in the service of art and fish. He and writer Brad Matsen have produced various books on their adventures with fish, both fossil and modern. Troll is currently completing a book on sharks. For an out-of-the-ordinary fish-viewing experience, see www.trollart.com.
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