The mystique of beachrock

ABSTRACT Parallel rows of intertidal beachrock composed of large (up to 4 m), oblong, pillowshape blocks submerged by rising Holocene sea level occur throughout the Caribbean. Such blocks have recently been discovered in 90 m of water off southwest Florida. The best known example is in 5-7 m of water off the northwest side of Bimini, Bahamas, where the feature is known as the Bimini Road. 'New-Age' alternative thinkers assert that the arrangement of the Bimini stones, and similar stones off Andros Island in the Bahamas, is actually man-made. The theory holds that ancient humans, principally citizens of the mythical city of Atlantis rearranged blocks of beachrock to form a harbour. This paper demonstrates that the stones and their arrangement are natural and suggests that some villages protected by ancient harbours in the Mediterranean may in fact have been developed on naturally occurring beachrock

Seepage meters and Bernoulli’s revenge,

ABSTRACT: Evaluation of seepage data from a network of 50 permanently deployed submarine seepage meters, specially constructed from fiberglass, indicates that the devices artificially advect (Bernoulli effect) shallow ground water. Reverse flow into the rock was not observed even when adjacent piezometers installed 2-m to 20-m below the rock-water interface indicated negative groundwater heads. Quantitative testing of five different designs, including conventional end-of-oildrum designs, indicates that meters presenting positive relief on the sea floor are subject to the Bernoulli effect when placed in areas where there are waves and/or currents. Advection does not appear to be caused by flexing of the collection bags

Seepage meters and Bernoulli’s revenge,

ABSTRACT: Evaluation of seepage data from a network of 50 permanently deployed submarine seepage meters, specially constructed from fiberglass, indicates that the devices artificially advect (Bernoulli effect) shallow ground water. Reverse flow into the rock was not observed even when adjacent piezometers installed 2-m to 20-m below the rock-water interface indicated negative groundwater heads. Quantitative testing of five different designs, including conventional end-of-oildrum designs, indicates that meters presenting positive relief on the sea floor are subject to the Bernoulli effect when placed in areas where there are waves and/or currents. Advection does not appear to be caused by flexing of the collection bags

Tracing the Mixing and Movement of Groundwater into Florida Bay with Four Naturally Occurring Radium Isotopes

Proceedings of the 1999 Georgia Water Resources Conference, March 30 and 31, Athens, Georgia.Four naturally occurring isotopes of radium (²²³, ²²⁴, ²²⁶, ²²⁸Ra) have a range in half-life that extends from a few days to over 1,600 years. Unique geochemical attributes make these radium isotopes ideal to examine sediment/water interface exchange processes in coastal waters. Here we present initial radium isotopic data of Florida Bay, a heavily impacted coastal system in south Florida. Florida Bay is a shallow, brackish, semi-enclosed water body that receives most of its limited freshwater supply from the Everglades, principally by surficial water runoff through Trout Creek/Taylor River. Because the entire region is underlain by highly porous Key Largo limestone and due to other hydrologic constraints, there is the possibility that ground water exchange may be significant in Florida Bay. To evaluate the extent of such a subsurface contribution, radium isotopes are being determined in shallow wells, seepage meter sites, and a series of water column samples across the Everglades National Park-Florida Bay boundary. All four radium isotopes were at least an order of magnitude greater in the two shallow well samples than in the water column samples. For example, ²²⁶Ra ranged from about 0.50 dpm L⁻¹ at a salinity of 5 to over 13 dpm L⁻¹ in Well B (salinity = 47.2). Isotopic radium ratios reveal that the well waters (i.e., marine ground water) are geochemically distinct from surficial waters and are regenerated on a time-scale of several days (i.e., ²²⁴Ra/²²³Ra). Results indicate that this radium quartet can be used effectively in Florida Bay to examine the exchange of surficial water and ground water.Sponsored and Organized by: U.S. Geological Survey, Georgia Department of Natural Resources, The University of Georgia, Georgia State University, Georgia Institute of TechnologyThis book was published by the Institute of Ecology, The University of Georgia, Athens, Georgia 30602-2202 with partial funding provided by the U.S. Department of Interior, geological Survey, through the Georgia Water Research Insttitute as authorized by the Water Research Institutes Authorization Act of 1990 (P.L. 101-397). The views and statements advanced in this publication are solely those of the authors and do not represent official views or policies of the University of Georgia or the U.S. Geological Survey or the conference sponsors

Efficacy, Immunogenicity and Safety of an Investigational Subunit Adjuvanted Herpes Zoster Vaccine in Adults Aged 60 Years and Older: Results From the ZOE-50 and ZOE-70 Efficacy Studies

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So What? A Brief History of Robert N. Ginsburg 1925-2017

This article summarizes the life and work of Robert Ginsburg

So What? A Brief History of Robert N. Ginsburg 1925-2017

This article summarizes the life and work of Robert Ginsburg

Seismic stratigraphy of the Blue Hole (Lighthouse Reef, Belize), a late Holocene climate and storm archive

Five seismic units may be identified in the similar to 8 m thick Holocene sediment package at the bottom of the Blue Hole, a 120 m deep sinkhole located in the atoll lagoon of Lighthouse Reef, Belize. These units may be correlated with the succession of an existing 5.85-m-long sediment core that reaches back to 1385 kyrs BP. The identification of seismic units is based on the fact that uniform, fine-grained background sediments show weak reflections while alternating background and coarser-grained event (storm) beds exhibit strong reflections in the seismic profiles. The main source of sediments is the marginal atoll reef and adjacent lagoon area to the east and north. Northeasterly winds and storms transport sediment into the Blue Hole, as seen in the eastward increase in sediment thickness, i.e., the eastward shallowing of the Blue Hole. Previous assumptions of much thicker Holocene sediment packages in the Blue Hole could not be confirmed. So far, close to 6-m-long cores were retrieved from the Blue Hole but the base of the sedimentary succession remains to be recovered. The nature of the basal sediments is unknown but mid-Holocene and possibly older, Pleistocene sinkhole deposits can be expected. The number of event beds identified in the Blue Hole (n = 37) during a 1.385 kyr-long period and the number of cyclones listed in historical databases suggest that only strong hurricanes (categories 4 and 5) left event beds in the Blue Hole sedimentary succession. Storm beds are numerous during 13-0.9 kyrs BP and 0.8-0.5 kyrs BP