Search Results - (Author, Cooperation:D. M. Bowman)

2015-04-04

Nature Publishing Group (NPG)

0028-0836

1476-4687

Biology

Chemistry and Pharmacology

Medicine

Natural Sciences in General

Physics

Arecaceae/*genetics ; Australia ; DNA, Plant/*genetics ; *Geographic Mapping ; Humans ; *Mythology ; Oceanic Ancestry Group/*psychology

2018-04-13

American Association for the Advancement of Science (AAAS)

0036-8075

1095-9203

Biology

Chemistry and Pharmacology

Geosciences

Computer Science

Medicine

Natural Sciences in General

Physics

Botany

2014-02-01

American Association for the Advancement of Science (AAAS)

0036-8075

1095-9203

Biology

Chemistry and Pharmacology

Computer Science

Medicine

Natural Sciences in General

Physics

Africa ; Australia ; *Climate ; *Ecosystem ; *Fires ; Humidity ; Models, Biological ; South America ; *Trees

1442-9993

Blackwell Publishing Journal Backfiles 1879-2005

Biology

Abstract  Soil organic matter (SOM) was sampled from lateritic soil profiles across an abrupt eucalypt savanna–monsoon rainforest boundary on the north coast of Croker Island, northern Australia. Accelerator mass spectrometry dating revealed that SOM that had accumulated at the base of these 1.5 m profiles had a radiocarbon age of about 5000 years. The mean carbon and nitrogen stable isotope composition of SOM from 10 cm deep layers from the surface, middle and base of three monsoon rainforest soil profiles was significantly different from the means for these layers in three adjacent savanna soil profiles, suggesting the isotopic ‘footprint’ of the vegetation boundary has been stable since the mid Holocene. Although there were no obvious environmental discontinuities associated with the boundary, the monsoon rainforest was found to occur on significantly more clay rich soils than the surrounding savanna. Tiny fragments of monsoon rainforest and abandoned ‘nests’ (large earthen mounds) of the orange-footed scrubfowl, an obligate monsoon rainforest species, occurred in the savanna, signalling that the rainforest was once more extensive. Despite episodic disturbances, such as tropical storm damage and fires, the stability of the boundary is probably maintained because clay rich soils enable monsoon rainforest tree species to grow rapidly and achieve canopy closure, thereby excluding grass and reducing the risk of fire. Conversely, slower tree growth rates, grass competition and fire on the savanna soils would impede the expansion of the rainforest although high rainfall periods with shorter dry seasons may enable rainforest trees to grow sufficiently quickly to colonize the savanna successfully.

Electronic Resource

1442-9993

Blackwell Publishing Journal Backfiles 1879-2005

Biology

The history of isolated patches of monsoon rainforest within large tracts of Eucalyptus savanna is poorly understood because of the scarcity of reliable palaeoecological records in the Australian monsoon tropics. Elsewhere in the world, the ratio of the stable isotopes 13C to 12C (δ13C) in soil organic matter has shed light on the dynamics of rainforest–savanna boundaries because tropical grasses with the C4 photosynthetic pathway have a distinct δ13C signature (–17 to –9‰) compared with that of woody plants with the C3 photosynthetic pathway (–32 to –22‰). In order to determine the magnitude of the variation in δ13C, unreplicated soil profiles were sampled beneath different vegetation types on three boundaries between Eucalyptus savanna and rainforest that were both growing on Tertiary age laterite parent material. Replicated (n = 3) soil profiles, which were also derived from Tertiary age laterite, were sampled from beneath: (i) dense stands of African grasses within a frequently burnt Eucalyptus savanna; and within the same long unburnt Eucalyptus savanna, (ii) patches of African and natives grasses and (iii) clumps of Acacia trees. The strongly negative δ13C values of soil organic matter derived from the frequently burnt and long unburnt grassy understoreys in the Eucalyptus savannas showed that a considerable amount of the soil carbon was derived from C3 (woody) species despite the presence of a ground layer dominated by C4 grasses. However, a feature of these data was the considerable variability among the three ‘replicate’ profiles. The surface soil samples from beneath three clumps of Acacia trees in the unburnt Eucalyptus savanna had much less variable δ13C values and were similar to two of the three monsoon rainforests sampled. The pattern of δ13C values from unreplicated soil profiles from different vegetation types across three rainforest boundaries was also very variable and not always obviously related the known disturbance history of the extant vegetation. Given the considerable variability within and between vegetation types with contrasting disturbance histories, it is concluded that the use of carbon stable isotopes to advance understanding of the dynamics of rainforest and Eucalyptus savanna boundaries will require further development, such as determination of the 14C age and δ13C values of different soil carbon fractions.

Electronic Resource

1573-5052

Aspect ; Eucalyptus ; Fire ; Forest ; Monsoon ; Northern Territory ; Radiation ; Rockiness

Springer Online Journal Archives 1860-2000

Biology

Abstract A model of direct and diffuse solar radiation on slopes of varying angle and aspect suggests that radiation differences within hilly terrain are maximized in the beginning of the dry season in the monsoon tropics. The differences between north and south facing slopes are greater than those found during the summer in the temperate zone. Within a study area near Mt. Bundey, Northern Territory, floristic and structural vegetational variability is closely related to June radiation as estimated by the model. However, the distribution patterns of monsoon thicket and eucalypt forest relate more to relative five protection than to the effects of incident radiation on temporal patterns of moisture availability. Within both major formations, site rockiness is an important influence on vegetation floristics and structure, both for five protection and through its influence on moisture availability.

Electronic Resource

1573-5052

Eucalypt forest ; Fire ; Floristic variation ; Laterite ; Monsoon thicket ; Monsoon tropics ; Northern Territory ; Soil moisture ; Stand structure ; Structural variation

Springer Online Journal Archives 1860-2000

Biology

Abstract A transect study of coastal forest vegetation on a lateritic peninsula in the Northern Territory revealed four distinct communities; eucalypt forest, mixed eucalypt forest-monsoon thicket, pure monsoon thicket and fringing coastal mangrove forest. The mangrove forest occurred in saline mud, the mixed and pure thicket on red earths and the eucalypt forest on both red and yellow earths. The eucalypt forest had less moisture in the surface soil than the other communities on the gentle slope above the mangroves. Evidence of past fire occurs in all the terrestrial communities, but the pure thicket is associated with a topographic position better protected from fire down-slope from the mixed community. Eucalypt regeneration in the mixed forest may be maintained by fires that have penetrated it from the frequently burnt eucalypt forest. It is possible that the mixed community is a fire sere occupying a site otherwise capable of supporting a pure thicket. However the pattern of vegetation has changed little in the recent past.

Electronic Resource

1573-5052

Eucalyptus tetrodonta ; Fire ; Gradient analysis ; Monsoon tropics ; Northern Australia ; Regeneration process ; Soil moisture ; Stand structure analysis ; Understorey variation

Springer Online Journal Archives 1860-2000

Biology

Abstract An ordination study of 20Eucalyptus tetrodonta forest stands growing on deep earths in monsoonal Australia revealed two major gradients in understorey vegetation type. The first axis reflected both floristic and structural understorey variation, where litter and shrub cover were inversely related to grass cover. This axis is thought to reflect a complex fire-vegetation type interaction, where vegetation is primarily determined by the saturation of the soil profile in the wet season, as measured by the colour of the iron rich soils. On the second axis of the ordination, floristic composition but not vegetation structure, and stand height were found to vary with the intercorrelated measures of soil gravel and moisture supply.E. tetrodonta is able to regenerate in the absence of fire, but firing appears to stimulate regeneration. All stands contained some advance growth, which occurs in distinct clumps, probably reflecting these plants clonal origin. Sapling presence in the stands is variable and the recruitment of advance growth into this size class appears to be related to over-wood competition. The size class distribution of trees was found to be similar amongst the stands, therefore stand structure appeared to be independent of understorey type. In comparison to general models of temperate eucalypt regeneration processes the tropical eucalypts have evolved different regeneration strategies, possibly in response to the severe annual drought.

Electronic Resource