Paul A. Colinvaux

A Long Pollen Record from Lowland Amazonia: Forest and Cooling in Glacial Times

A continuous pollen history of more than 40,000 years was obtained from a lake in the lowland Amazon rain forest. Pollen spectra demonstrate that tropical rain forest occupied the region continuously and that savannas or grasslands were not present during the last glacial maximum. The data suggest that the western Amazon forest was not fragmented into refugia in glacial times and that the lowlands were not a source of dust. Glacial age forests were comparable to modern forests but also included species now restricted to higher elevations by temperature, suggesting a cooling of the order of 5° to 6°C.

A 14 300-Yr Paleoecological Profile of a Lowland Tropical Lake in Panama

The first paleoecological analysis of a complete sedimentary record spanning the period from the late Pleistocene to the present from lowland Panama, documents changes in lowland vegetation communities through major climatic change and the onset of human disturbance. Past sympatry is found among presently allopatric species, suggesting that tropical forest communities are not species-stable through time. Late Pleistocene floras at Lake La Yeguada (elevation 650 m), Panama, had high relative abundance of montane forest elements, e.g., Quercus and Magnolia, existing some 900 m below their present range, suggesting a climatic cooling of - 50C below present. This descent of montane forest taxa onto lowland hilltops denied the ground to postulated lowland rain forest refugia. The late Pleistocene (14 350-11 050 yr BP) was not uniformly cool and was interrupted by brief phases of near present-day warming. The onset of the Holocene was abrupt, taking < 100 yr, and was almost coincidental with the start of human forest disturbance. Changes in climate at La Yeguada were found to be largely synchronous with those documented at Lake Valencia, Venezuela, but no fine-scale climatic synchrony was apparent with South American or European sites, and significant departures from the predictions of published climatic circulation models are found.

Late pleistocene temperature depression and vegetation change in Ecuadorian Amazonia

Abstract Paleoecological (pollen, phytolith, and wood) analyses of sediments, radiocarbon dated 33,000 to 26,000 yr B.P., from two sites in Ecuadorian Amazonia provide data that suggest a cooling of ca. 7.5°C below present in equatorial lowlands from 33,000 to 30,000 yr B.P. A period of warning followed in which novel species assemblages, a blend of montane and lowland floral components, persisted for at least 4000 years. These data of forest community change, from sites lying within the postulated glacial rain forest Napo refugium, provide the strongest paleoecological refutation of the refugial hypothesis yet obtained. The large temperature depression at ca. 30,000 yr B.P. allows the possibility that if maximum cooling at the equator was synchronous with the last glacial maximum (LGM) of the northern hemisphere, freezing temperatures would have been experienced in parts of lowland Amazonia between 25,000 and 18,000 B.P.

A pollen record of a complete glacial cycle from lowland Panama

A long pollen record from lowland Panama describes the vegetation during glacial times and proba- bly includes a history of the last 150 000 yr, thus represen- ting a complete glacial cycle. The record is from sedi- ments of an extinct caldera lake under the town of El Valle. Throughout most of the last glacial period oaks and other plants of the modem montane forest maintained sig- nificant populations about 700 m lower than present. Im- mediately before the 14 000 B.P. start of the late glacial period oaks had reached to 1000 m below present limits. These data require significant temperature depressions, perhaps in the order of 4 - 6 ?C at some seasons of the year. Lowland forest taxa persisted in the neighbourhood of El Valle throughout the glacial period, however, suggesting reassortment of plant populations into communities with- out modem analog. Although our reconstruction of levels of the El Valle lake in the period 30 000 to 12 000 B.P. suggests less precipitation than in modem times, the lowland climate appears to have been moist enough for taxa of tropical forests to persist. The montane floras of the western and eastern Panama highlands did not merge at any time in the glacial cycle and an hypothesis of dispersal between enlarged areas of montane forest is put forward to explain modem disjunctions in Quercus distri- butions. The wet highlands of Panama were never refugia for tropical rain forest taxa at any time during the Quater- nary, rather rain forest species existed in unfamiliar communities in the Panamanian lowlands.

Amazon diversity in light of the paleoecological record

Abstract Disjunct distributions of Amazonian species have been explained previously by a refugial theory which postulates that Amazonian rain forest was preserved in large highland regions throughout the Pleistocene. No direct, radiocarbon dated evidence exists for the last glacial maximum with which to test this theory. The only radiocarbon dates of Pleistocene age from the Amazon basin are of fossiliferous deposits in the proposed Napo refugium of the West, where both pollen assemblages and wood samples indicate that forest with cool Andean elements existed there at two intervals in the last cycle of northern hemisphere glaciation, implying a temperature depression of at least 4°C in the Amazon lowlands. Under modern climatic conditions, lateral erosion by river meander, together with surface erosion, serves as a rejuvenating mechanism for the rain forests of Peru and Ecuador. The instability of late Holocene Amazonian climates is demonstrated by documenting a precipitation event in the eastern Andean cordillera that caused widespread flooding of western Amazonian forests 800–1300 BP. Late Holocene pollen histories from widely dispersed parts of central Amazonia distinguish between vegetation histories in the drainage of northern, south-western and western watersheds, but all show histories of fluctuating intensities of dry seasons. Radiocarbon dating of charcoal layers in soils of Venezuelan Amazonia demonstrates the apparently random incidence of wild fires at wide intervals over at least the last 6 ka. The high species richness of Amazonia is a result of numerous opportunities for vicariance because of a very large total area, wide variety of habitats and intermediate levels of disturbance, particularly by hydrological processes, that has varied on timescales from years to millennia. Amazonian disjunct distributions probably reflect regional environmental discontinuities in both interglacial and glacial times.

Paleoenvironments and human occupation in late-glacial Panama

The first pollen and phytolith data covering the entire Pleistocene/Holocene transition from the lowlands of the Central American isthmus indicate that the forests of late-glacial Panama at an altitude of 650 m resembled those currently found at ca. 1500–1800 m. A temperature depression of ca. 5°C and reduced precipitation/evaporation ratios in the late-glacial period are suggested. Forest composition from ca. 14,000 to 10,500 yr B.P., although primarily montane in character, contained a low biomass of species today segregated in lowland forests and, hence, a floral assemblage with no modern analog. The sudden appearance of carbon and burnt, weedy plant material at ca. 11,000 yr B.P. is attributed to the earliest human impact yet recorded from tropical America and may perhaps have been associated with the first human occupation of the region.

Tropical Forest Disturbance: Paleoecological Records from Darien, Panama

The first paleoecological data from the Darien of Panama, a remote region rich in endemic species and purported to be one of the last untouched neotropical wilderness, demonstrate a 4000—yr history of human disturbance. Unstable climate is recorded as changes in precipitation inferred from the diatom record, but a more important source of disturbance has been human activity. Pollen, and phytoliths of Zea mays, and charcoal from grass fires confirm historical and archaeological judgments that the region has a long history of human settlement.The data are consistent with depopulation and abandonment of most agriculture following the Spanish conquest, showing that the local modern forest has developed in recent centuries. Four millennia of disturbance that preceded the decline of human populations may have had a profound effect upon the modern forest associations. The apparently pristine forests appear to have regrown in just 350 yr, probably from populations fragmented by previous agricultural disturbance. ...

Temperature depression in the Lowland Tropics in glacial times

Equatorial air temperatures at low elevations in the New World tropics are shown by pollen and other data to have been significantly lowered in long intervals of the last glaciation. These new data show that long recognized evidence for cooling at high elevations in the tropics were symptomatic of general tropical cooling and that they did not require appeal to altered lapse rates or other special mechanisms to be made to conform with conclusions that equatorial sea surface temperatures (SSTs) were scarcely changed in glacial times. The new data should be read in conjunction with recent findings that Caribbean (SSTs) were lowered in the order of 5 ° C, contrary to previous interpretations. Thus these accumulating data show that low latitudes as well as high were cooled in glaciations. In part the earlier failure to find evidence of low elevation cooling in the lowland tropics resulted from the data being masked by strong signals for aridity given by old lake levels in parts of Africa and elsewhere. Global circulation models used to predict future effects of greenhouse warming must also be able to simulate the significant cooling of the large tropical land masses at glacial times with reduced greenhouse gas concentrations. Plants and animals of the Amazon forest and similar ecosystems are able to survive in wide ranges of temperatures, CO2 concentrations, and disturbance, though associations change constantly.

Orbital forcing signal in sediments of two Amazonianlakes

Paleolimnological data from two ancient lakes at 0° latitudein Amazonia indicate that past lake level changes reflect precessional (19,000to 22,000 years) variations in insolation over the last 170,000 years. Waterlevel in Lakes Pata and Verde, Brazil, is determined by the ratio ofprecipitation:leakage. Times of low lake level are indicated in sediments byoxidized clays, evidence of algal blooms and high K+ concentrations.Peak K+ values are attributed to biogenic concentration when thelake was reduced to a shallow, productive pool. Low lake phases correlate withmaximum insolation during the dry season (June–July–August). Thusthe last glacial maximum 18,000 to 22,000 yr BP was a wet time in northernAmazonia, and the driest period of the last 170,000 years was from 35,000 to27,000 yr BP. These results from near the equator do not imply thatprecipitation changed synchronously across Amazonia, because geographiclocations throughout the vast watershed were undoubtedly influenced by localmoisture sources.

A 7000-year pollen record from the Amazon lowlands, Ecuador

The longest continuous Amazonian palynological record (ca 7010 yrs B.P. to present) from Lake Ayauchi, Ecuador, reveals species-by-species abundance changes during a period of climatic change. Pollen influx from a wet tropical rain forest was found to be high, 1×104−105 grains cm-2 yr-1, although mature forest taxa were poorly represented. Horizons of laminated sediments and weathered gyttja, dated to ca 4200–3150 B.P., evidence a period of reduced net water availability. During this period Ficus, Alchornea and Palmae pollen representation appears to decline, although there is no evidence of a major forest compositional change. The lake was reduced to a shallow, possibly seasonal, pool. Zea cultivation was recorded between ca 2850 B.P., (the earliest paleoecological record to date in the Amazon basin) and ca 800 B.P. It is suggested that Zea was cultivated on exposed lake sediment within the crater at times of low water levels. The abandonment of Zea cultivation may have been due to rising water levels or social unrest.