Pattern and Process in Arid-Region Salt Marshes — Southern California

Author(s):  
Christopher P. Onuf ◽  
Joy B. Zedler
2004 ◽  
Vol 7 (2) ◽  
pp. 107-124 ◽  
Author(s):  
John C. Callaway ◽  
Joy B. Zedler

2000 ◽  
Vol 14 (3) ◽  
pp. 233-252 ◽  
Author(s):  
J.S Desmond ◽  
J.B Zedler ◽  
G.D Williams

2015 ◽  
Vol 114 (1) ◽  
pp. 22-32
Author(s):  
Jason K. Keller ◽  
Tyler Anthony ◽  
Dustin Clark ◽  
Kristin Gabriel ◽  
Dewmini Gamalath ◽  
...  

2010 ◽  
Vol 7 (11) ◽  
pp. 3657-3668 ◽  
Author(s):  
E. Blei ◽  
M. R. Heal ◽  
K. V. Heal

Abstract. Fluxes of CH3Br and CH3Cl and their relationship with potential drivers such as sunlight, temperature and soil moisture, were monitored at fortnightly to monthly intervals for more than two years at two contrasting temperate salt marsh sites in Scotland. Manipulation experiments were conducted to further investigate possible links between drivers and fluxes. Fluxes followed both seasonal and diurnal trends with highest fluxes during summer days and lowest (negative) fluxes during winter nights. Mean (± 1 sd) annually and diurnally-weighted net emissions from the two sites were found to be 300 ± 44 ng m−2 h−1 for CH3Br and 662 ± 266 ng m−2 h−1 for CH3Cl. The fluxes from this work are similar to findings from this and other research groups for salt marshes in cooler, higher latitude climates, but lower than values from salt marshes in the Mediterranean climate of southern California. Statistical analysis generally did not demonstrate a strong link between temperature or sunlight levels and methyl halide fluxes, although it is likely that temperatures have a weak direct influence on emissions, and both certainly have indirect influence via the annual and daily cycles of the vegetation. CH3Cl flux magnitudes from different measurement locations depended on the plant species enclosed whereas such dependency was not discernible for CH3Br fluxes. In 14 out of 18 collars with vegetation CH3Br and CH3Cl net fluxes were significantly positively correlated. The CH3Cl/CH3Br net-emission mass ratio was 2.2, a magnitude lower than mass ratios of global methyl halide budgets (~22) or emissions from tropical rainforests (~60). This is likely due to preference for CH3Br production by the relatively high bromine content in the salt marsh plant material. Extrapolation based solely on data from this study yields salt marsh contributions of 0.5–3.2% and 0.05–0.33%, respectively, of currently-estimated total global production of CH3Br and CH3Cl, but actual global contributions likely lie between these values and those derived from southern California.


PLoS ONE ◽  
2020 ◽  
Vol 15 (11) ◽  
pp. e0240597
Author(s):  
Kaelin J. McAtee ◽  
Karen M. Thorne ◽  
Christine R. Whitcraft

The implementation and monitoring of management strategies is integral to protect coastal marshes from increased inundation and submergence under sea-level rise. Sediment addition is one such strategy in which sediment is added to marshes to raise relative elevations, decrease tidal inundation, and enhance ecosystem processes. This study looked at the plant and invertebrate community responses over 12 months following a sediment addition project on a salt marsh located in an urbanized estuary in southern California, USA. This salt marsh is experiencing local subsidence, is sediment-limited from landscape modifications, has resident protected species, and is at-risk of submergence from sea-level rise. Abiotic measurements, invertebrate cores, and plant parameters were analyzed before and after sediment application in a before-after-control-impact (BACI) design. Immediately following the sediment application, plant cover and invertebrate abundance decreased significantly, with smothering of existing vegetation communities without regrowth, presumably creating resulting harsh abiotic conditions. At six months after the sediment application treatment, Salicornia bigelovii minimally colonized the sediment application area, and Spartina foliosa spread vegetatively from the edges of the marsh; however, at 12 months following sediment application overall plant recovery was still minimal. Community composition of infaunal invertebrates shifted from a dominance of marsh-associated groups like oligochaetes and polychaetes to more terrestrial and more mobile dispersers like insect larvae. In contrast to other studies, such as those with high organic deposition, that showed vegetation and invertebrate community recovery within one year of sediment application, our results indicated a much slower recovery following a sediment addition of 32 cm which resulted in a supratidal elevation with an average of 1.62 m (NAVD88) at our sampling locations. Our results indicate that the site did not recover after one year and that recovery may take longer which illustrates the importance of long-term monitoring to fully understand restoration trajectories and inform adaptive management. Testing and monitoring sea-level rise adaptation strategies like sediment addition for salt marshes is important to prevent the loss of important coastal ecosystems.


1936 ◽  
Vol 1 (4) ◽  
pp. 295-300 ◽  
Author(s):  
Elizabeth W. Crozer Campbell

During years of painstaking work in the California Desert certain types of flint implements seem to have occurred again and again. Our work is now carried on with two main objectives: one to cover all likely areas where sites might be found, the other to try to discover if cultural groups follow certain geologic formations and if so, to place these types in their proper sequence, all of which is no very simple task. With these two main objectives in view, it is proposed to scour the more arid region of southern California, with the idea that any solution of the problems connected with this territory may prove a possible clew towards unraveling the story of prehistoric man in wider portions of the Great Basin, which we hope to explore in the future.


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