Is Sahara Desert several million years older than previously thought?

Sahara desert. Credit: © mrks_v / Fotolia

A team of scientists from Norway, France and China have revised the view that the Sahara desert has existed for only the last 2 to 3 million years.

The Sahara is the world's largest subtropical desert. During the last decades, numerous scientific studies have probed its geological and archeological archives seeking to reveal its history. Despite some important breakthroughs, there are still basic questions that lack satisfactory answers.

For example, how old is the Sahara desert? It is widely believed that Sahara desert first appeared during the last 2 to 3 million years, but recent discoveries such as ancient sand dunes and dust records in marine cores push the possible onset of Saharan aridity back in time by several million years. Until now, however, there have been no good explanations for such an early Sahara onset.

This study pinpoints the Tortonian stage (~7-11 million years ago) as a pivotal period for triggering North African aridity and creating the Sahara desert. Using snapshot simulations with the Norwegian Earth System Model (NorESM) model suite, the international team explored the climate evolution of North Africa through major tectonic shifts over the last 30 million years. They found that the region undergoes aridification with the shrinkage of the Tethys -- a giant ocean that was the origin of the modern Mediterranean, Black and Caspian Seas -- during the Tortonian.

The simulations are the first to show that the Tethys shrinkage has two main consequences for North African climate. First, it weakens the African summer monsoon circulations and dries out North Africa. Second, it enhances the sensitivity of the African summer monsoon and its associated rainfall to orbital forcing. The Tortonian stage thus marks the time when North Africa shifted from a permanently lush, vegetated landscape to a landscape experiencing arid/humid cycles on orbital time scales.

Interestingly, these major changes in North African climate and environment are coincident with an important time period for the emergence of early hominids.

Source: Uni Research

Desert streams: Deceptively simple

Dryland channels exhibit very simple topography despite being shaped by volatile rainstorms. Credit: Katerina Michaelides

Volatile rainstorms drive complex landscape changes in deserts, particularly in dryland channels, which are shaped by flash flooding. Paradoxically, such desert streams have surprisingly simple topography with smooth, straight and symmetrical form that until now has defied explanation.

That paradox has been resolved in newly published research conducted by Michael Singer and Katerina Michaelides, associate researchers at UC Santa Barbara's Earth Research Institute. The pair show that simple topography in dryland channels is maintained by complex interactions among rainstorms, the stream flows these storms generate in the river channel and sediment grains present on the riverbed. Their findings appear in the journal Geology.

Desert streams flow only during infrequent but intense rainstorms, and when they do, only parts of the channel contain water, making the flow irregular and erratic. One rainstorm may erode sediment grains in one section of the channel, while another storm moves sediment in a different area.

"Given this localized sediment movement during rainstorms, one might expect desert channels to contain mounds of sediment that undulate down the stream course reflecting the irregular flow, but they don't," Singer said. "The water produced in the channel only flows partially down the stream and then stops because it seeps into the riverbed, and there's not enough water from upstream to replace it, so it just disappears."

Because desert river channels do not feature the river bars, pools or riffles common in perennial streams, they decline in elevation downstream very smoothly. According to the researchers' findings, feedback between two variables -- complex water and sediment movements -- shape such basins.

Singer and Michaelides used data collected from the Rambla de Nogalte in southeastern Spain to model these dryland channel variables. The area has a semi-arid climate with mean annual rainfall of around 14 inches, which occurs during convective rainstorms, producing large floods that recur about once a decade.

They found that dryland channel width fluctuates downstream. Their observations show that grain size (roughness) also fluctuates from sand to gravel a downstream direction.

"There's feedback between this fluctuating width and fluctuating grain size," Singer said. "The stream flow is generated in a discontinuous pattern along the channel. Some rainstorms produce a bit of topography in some parts of the channel. Other spatial configurations of flow generated by storms destroy that topography so the variability of the rainstorms interacting with this channel are creating and destroying the topography constantly to keep it in this simple form."

Singer and Michaelides also produced simulations of extreme flows to determine the volume of flow necessary to reshape the channel completely. They examined the longitudinal variability of sediment flow as well as sediment storage to find the channel-shaping threshold. This threshold reshapes the entire channel and makes it smooth again. "It's a really significant threshold that tells us the magnitude of the flood necessary to reshape the channel," Singer said.

"Semi-arid and arid river systems are extremely important to the populations that live around them," he concluded. "Water resources are obviously a huge limitation in the development of societies, and a lot of water is being progressively diverted for irrigation, water use and other purposes, so those can further affect the spatial patterns of where flow is in these channels and potentially impact the processes of where topography develops in the river channel. Humans can inadvertently have an impact on the shape and form of river channels like these."

Source:  University of California - Santa Barbara

Scale of declines of UK migratory birds wintering in Africa revealed

Yellow Wagtails have declined in the UK by 43% since 1995. Credit: Andy Hay; rspb-images.com

The migration of millions of birds across the face of the planet is one of nature's greatest annual events. Every spring some species move in one direction, while every autumn those same species move in the opposite one, very often linking continents.

Although these migration patterns are as regular as the seasons, monitoring is revealing that, for some species, fewer birds are making the journey each season as the populations of these birds, including species nesting in the UK, are declining rapidly.

The latest in the annual series of State of the UK's Birds report includes a migratory birds section, including trends for 29 migrant species which nest in the UK in summer and spend the winter around the Mediterranean, or in Africa south of the Sahara Desert. For the first time the recent population trends for these migratory species have been combined into an indicator revealing some marked differences between species that winter in different areas.

Species, such as Whinchat, Common Nightingale, Tree Pipit and Spotted Flycatcher, which winter in the humid zone of Africa -- stretching across the continent from southern Senegal to Nigeria and beyond -- show the most dramatic declines: the indicator for this group of species has dropped by just over 70% since the late 1980s. This contrasts with species, such as Sand martin, Common Whitethroat and Sedge Warbler, wintering in the arid zone (just below the Sahara desert). These species have fluctuated considerably since 1970, but show a less than 20% decline overall.

One of the most dramatic declines is that of the European Turtle-dove with a decline of 88% since 1995. The following species have also declined over the same period: Wood Warbler, 66%; European Pied Flycatcher, 53%; Spotted Flycatcher, 49%; Common Cuckoo, 49%; Common Nightingale, 43%; and Yellow Wagtail, 43%.

Concern about migratory bird species is growing and future editions of the State of the UK's Birds report will contain a regular update to the migratory bird indicator. To understand the changing status of the UK's migratory birds, researchers need to understand more about what's driving these declines. Evidence is currently being gathered from a variety of sources including tracking studies and on-the-ground surveys.

Martin Harper, RSPB Conservation Director, said: 'West Africa is the winter home for many species bird species that breed in the UK. But many of these birds that cross continents are in rapid decline. Their nomadic lifestyle, requiring sites and resources spread over vast distances across the globe makes identifying and understanding the causes of decline extremely complex.

'The problems may be in the UK or in West Africa, or indeed on migration in between the two.'

David Noble, Principal Ecologist at the British Trust for Ornithology (BTO), said: 'We can accurately monitor the patterns of decline in these once-familiar summer breeders thanks to several decades of careful observations by an army of volunteer birdwatchers. More recently, tracking devices have shed light on migratory routes and key wintering areas.

'To take appropriate action, further study is needed to determine the pressures faced in sub-Saharan Africa, as well as breeding here in the UK.'

Colette Hall, Wildfowl & Wetlands Trust (WWT) Species Monitoring Officer, said: 'The length of many bird migrations -- often thousands of miles -- makes it very difficult to pinpoint where and what is causing populations to fall.

'So the more information we can get all along the migration routes -- on land use changes, new infrastructure etc -- the better we can target protection measures. It's important that we help build up the capacity of local bird organisations and volunteers across the world to provide vital information through their own long-term monitoring.'

Alan Law, Director of Biodiversity Delivery at Natural England said: 'It is self-evident that effective conservation of a migratory species requires appropriate measures to be in place at each step of the migratory cycle.

'For some species, there is growing evidence of pressure on breeding success here in England. Our focus therefore is to ensure that well-managed habitats are available in this country so that migratory species can breed here successfully; this work involves close collaboration with land managers both on designated conservation sites and across the wider farmed countryside.'

David Stroud, Senior Ornithologist with the Joint Nature Conservation Committee, said: 'Migratory birds depend on conservation actions in all the countries they move through in the course of their annual cycle.

'The UK is working with these countries to help improve the condition of their critical habitats through its participation in multi-lateral environmental agreements such as the Biodiversity Convention and the Ramsar Convention on wetlands.'

The State of the UK's Birds report also covers the UK's Overseas Territories. The latest evidence reveals mixed fortunes for two important albatross populations in the UK's Overseas Territories. Seventy per cent of the world's Black-browed Albatrosses nest in the Falkland Islands. A population increase here has allowed researchers to downgrade the extinction threat of this species from Endangered to Near Threatened. Sadly, the fortunes of the Grey-headed Albatross has deteriorated as declines have been reported in nesting colonies on South Georgia, which hosts half the world's population.

The State of the UK's Birds report is available online at: http://www.rspb.org.uk/Images/state-of-the-uks-birds_tcm9-383971.pdf

Source: BirdLife International

Centuries of sand still available at Mississippi Delta

These satellite images show a portion of the Mississippi River downstream of Memphis, Tenn., in August 2012 (top) and August 2011 (bottom). During the drought of 2012, record low-water levels revealed vast amounts of sand that are typically hidden below water. New research finds that the river’s supply of sand — the material engineers most need to rebuild the shrinking Mississippi Delta — will stay constant for centuries.

The wetlands of the Mississippi River Delta are slowly sinking and rapidly eroding, but new research from Rice University and the University of South Carolina has found the river's supply of sand -- the material engineers most need to rebuild the delta -- will stay constant for centuries.

The new study, which appears online this week in Nature Geoscience, is encouraging news for scientists and government officials who are working to shore up southeastern Louisiana's rapidly disappearing wetlands. The delta sinks each year as its soil settles and becomes more compact. While floodwaters from the untamed Mississippi River formerly provided a steady supply of sediment to counteract this subsidence, engineers have fought for nearly a century to contain the floods, which threaten the lives and livelihood of millions. Flood-control measures have eliminated about half of the annual supply of sediment that flows downriver, but the new study finds that sand -- they key ingredient for rebuilding marshlands -- is still abundant.

"It's true that the total amount of sediment has diminished, but river sediment contains both fine-grained mud and course-grained sand, and our research found that upstream dam construction has not reduced the amount of sand in the lower Mississippi and won't for at least 300-600 years," said study lead author Jeffrey Nittrouer, assistant professor of Earth science at Rice University.

Nittrouer and co-author Enrica Viparelli, assistant professor of civil and environmental engineering at the University of South Carolina, analyzed sediment loads in the lower Mississippi and found that while the total amount of sediment -- both sand and mud -- has diminished, the amount of sand trapped by upstream dams is offset by "mining" of new sand downstream.

"When clear water is released from the floodgates at upstream dams, it churns dormant sand that has long been deposited and carries it downriver," Nittrouer said. "This 'mining' of ancient sand makes up for the sand that is trapped by upstream dams, and our numerical models suggest that the sand load in the lower Mississippi River channel will not decline for at least 300 years. Looking even further into the future, we found that 600 years from now, the lower Mississippi River's sand sediment load will have declined by less than 20 percent from today's levels."

Nittrouer, whose research focuses on the sediment transport, hydrology, basin evolution and stratigraphy of lowland river systems, has studied the Mississippi River for the past decade. His previous work included a 2012 study of the land-building processes that took place during the historic flooding of 2011. In one of the largest floodwater diversions of the past century, the U.S. Army Corps of Engineers opened the Bonnet Carré Spillway, a 7,000-foot-wide "safety valve" that diverts floodwater directly to Lake Ponchatrain.

Nittrouer and colleagues found that even though the 42-day diversion siphoned off less than 20 percent of the water flowing downriver, it diverted about 40 percent of the river's sand load into Bonnet Carré. In analyzing how this occurred, Nittrouer and colleagues were able to show what factors the corps should consider in designing sediment diversion projects for wetlands replenishment.

"Our previous work showed how large volumes of sand could be deposited in specific locations, and our latest research shows that significant volumes of sand will be available for land-building for several centuries," Nittrouer said. "Each of these are important because studies at Wax Lake Delta and other sites have shown that sand -- even though it makes up less than 20 percent of the overall river sediment load -- is the key ingredient for land-building."

Source: Rice University