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Cell Polarity Ing news and views ment of the RAFOS float speeds to results of N a e e the MODAS — Modular Ocean Data Assimi- o t r r S B th ia e ra d d t zi e e a l C R w lation System — model, which assimilates 0° . rm te Benguela in satellite altimetric measurement of sea-level undercurrent variability. m ic o f fr i Benguela C. r c There is still a great deal to learn about the a te a P e Agulhas valve, and its variation under differ- ° il W h 30 S z nt Cape t a e r r Agulhas Current ent climatic conditions. Ensuring that it is r Cauldron B u C properly represented in global ocean and cli- mate models remains a daunting challenge. South Atlantic Agulhas return current ke rrent 2 ra e Cu Agulhas retroflection But this collection of papers shows how the ° D ag 60 S ss Pa brotherhood of observers armed with new tools, aided by satellite-based remote sens- 60°W0° 60°E 120°E ing, and modellers with their increasingly realistic simulations, can take us forward. ■ Figure 1 The Agulhas system and associated flow patterns. The Agulhas Current draws water from the Arnold L. Gordon is at the Lamont–Doherty Earth Pacific Ocean through the Indonesian throughflow and Drake Passage, and from the Tasman Sea. It Observatory, Columbia University, Palisades, New abruptly turns back towards the Indian Ocean near 20° E. Here, at the Agulhas retroflection, ‘leakage’ York 10964, USA. of water occurs within an array of cyclonic (clockwise) and anticyclonic (anticlockwise) eddies that e-mail: [email protected] are injected into the vigorous stirring and mixing environment of the Cape Basin (the ‘Cape 1. Bang, N. D. S. African Geog. J. 52, 67–76 (1970). Cauldron’). The South Atlantic Current adds water to the cauldron, as does the subsurface flow of 2. Richardson, P. L. (ed.) Deep-Sea Res. II 50, 1–319 (2003). 3. Matano, R. P. J. Phys. Oceanogr. 26, 2267–2279 (1996). the Benguela undercurrent along the west coast of Africa, and salty Red Sea water along the east 4. Reason, C. J. J. Clim. 14, 2769–2778 (2001). coast. A blend of these waters spreads into the Brazil and North Brazil currents. The latter is part of 5. Gordon, A. L. J. Geophys. Res. 91, 5037–5046 (1986). the large-scale ‘overturning circulation’ induced by the formation of North Atlantic Deep Water. 6. Gordon, A. L. in Ocean Circulation and Climate (eds Siedler, G., Church, J. & Gould, J.) 303–314 (Academic, 2001). 7. de Ruijter, W. A. et al. J. Geophys. Res. 104, 20885–20910 (1999). powerful eddies, 100–400 km in diameter. All Brazil Current, as part of the NADW over- 8. Gordon, A. L., Weiss, R. F., Smethie, W. M. Jr & Warner, M. J. of these eddies are generated within or along turning circulation. About three Agulhas J. Geophys. Res. 97, 7223–7240 (1992). the periphery of the retroflection, some of rings shed from the retroflection survive the 9. Sloyan, B. M. & Rintoul, S. R. J. Phys. Oceanogr. 31, 1005–1030 (2001). them originating from the Indian Ocean, blender, and make stately progress over the 10.Gordon, A. L. & Fine, R. A. Nature 379, 146–149 (1996). others from the South Atlantic Current (Fig. mid-ocean ridge and into the western South 11.Speich, S. et al. Geophys. Res. Lett. 29, 10–13 (2002). 1). These eddies are not just large anticyclonic Atlantic Ocean. There, three to four years 12.Beal, L. M., Ffield, A. & Gordon, A. L. J. Geophys. Res. Oceans 105, 8549–8564 (2000). rings, cast off from the retroflection at an later, they will impinge upon the Brazil Cur- 13.Weijer, W., de Ruijter, W. P. M. & Dijkstra, H. A. J. Phys. average rate of six per year. Rather, they are a rent. It is encouraging to note the close agree- Oceanogr. 31, 2385–2402 (2001). hodgepodge of types, which interact with each other and with the main retroflection, in a general milieu of vigorous stirring and mix- Cell polarity ing. Indian Ocean water is trapped within the eddy cores, and is often lost in the process, blending into the regional background (this From embryo to axon is usually ‘thermocline water’ — that is, water Melissa M. Rolls and Chris Q. Doe from above about 800-m depth — but can take in the upper kilometre or two). Many cell types in our body, ranging from neurons to the epithelial cells Studies of specific, newly formed Agulhas that line the lungs and skin, must be polarized to function properly. The rings have exposed their turbulent birth and same mechanism may establish the polarity of many of these cells. early evolution as they drift into the caul- dron, with numerical simulations adding ow are we to make sense of the com- Writing in Cell, Shi and colleagues1 provide further detail to our picture of the complex plexity of our brains? Filled with clues to the process; their results point to a Cape Basin circulation. These simulations Hbillions of nerve cells, each making mechanism for establishing cell polarity that can resolve quite fine-grained behaviour, hundreds or thousands of precise connec- functions from embryos to axons. and they reveal the coexistence, in dipoles, of tions to other neurons, this organ develops Until now, two classes of proteins have anticyclonic eddies intensified at the surface anew in each of us. Not only that, but if you been implicated in establishing neuronal with cyclonic partners intensified at the sea were to take a closer look at the individual polarity. The first class is involved in remod- floor. The cyclonic eddies are caged in by the cells, you would see that they come in thou- elling actin filaments, one of the major com- topography of the Cape Basin. But the anti- sands of stunning shapes. But there is a ponents of the cellular ‘skeleton’. Actin cyclonic eddies can break out of the basin theme that emerges from studying these remodelling must take place during any and enter the South Atlantic, although with shapes. In vertebrates, most neurons have a change in cell shape, such as axon or dendrite substantial energy loss. single long protrusion, the axon, that is protrusion, and is particularly important Other authors in the special issue2 describe specialized to transmit signals to other cells, during the initial steps of axon formation2. how the witch’s brew of the Cape Cauldron as well as many shorter, branched protru- The proteins in question include the Rho feeds blended water, via the Benguela Cur- sions called dendrites that are specialized to family of enzymes, and are thought to enable rent, into the subtropical gyre of the South receive signals (Fig. 1). Perhaps understand- the rapid growth required by an extending Atlantic. Some of this water remains within ing this fundamental polarity would be a axon3. The second class of proteins includes the gyre, eventually finding its way back to the good starting point for understanding the modulators of another type of cytoskeletal Indian Ocean in what can be thought of as a brain’s complexity. Over the past few years, filament, microtubules. Proteins in this class super-subtropical gyre spanning the South progress has been made in defining how are either unique to, or used differently by, Atlantic and Indian Oceans. But some enters axons and dendrites differ. But less is known neurons. Axons are enriched in several neu- the Northern Hemisphere within the North about how they are initially established. ron-specific microtubule-binding proteins, NATURE | VOL 421 | 27 FEBRUARY 2003 | www.nature.com/nature © 2003 Nature Publishing Group 905 news and views Axon polarity of the fertilized egg. Par-3 and Par-6 localize together with another enzyme, in particular seem to be part of an evolution- atypical protein kinase C, and Shi et al. also arily conserved protein complex that con- provide pharmacological evidence that this trols polarity in a range of cell types5,6 (Fig. enzyme has a role in axon outgrowth. They 2). In worms these two proteins localize to suggest that this might be due to an effect on the anterior of the fertilized egg, and coordi- microtubule dynamics. nate aspects of cell polarity that ultimately Another interesting set of questions per- distinguish the head and the tail of the adult tains to the very earliest events of axon out- wiggling worm. In organisms from mam- growth. What triggers the loss of Par-3 and mals to fruitflies, Par-3 and Par-6 are distrib- Par-6 from immature neurites and their uted asymmetrically in epithelial cells enrichment in the developing axon? Here (which line the stomach, lungs and skin, for studies of other systems provide few clues, instance). Here, the Par proteins are distrib- because little is known about how Par-3 and uted to the cellular apical side — which faces Par-6 become localized in any cell type. It is the outside world, in these examples the air also unknown how the timing of Par-3/Par-6 or stomach contents — helping to distin- localization in cultured neurons, which lack guish it from the basal surface. In addition, normal environmental cues, relates to the Par-3 and Par-6 control the polarity of neural situation in vivo. precursors in many organisms. Can we learn anything from the presence 1 Information Shi et al. have now looked at the role of of Par-3 and Par-6 in developing axons about Par-3 and Par-6 in determining the polarity the flip side of neuronal polarity: the specifi- of neurons from the hippocampal brain cation of dendrites? Perhaps these proteins region in rats.
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