Malayomaorica malayomaorica is an important Upper Jurassic bivalve in the southern hemisphere: widely distributed in strata of Early – Middle Kimmeridgian age, it is a zone fossil of considerable potential for regional biostratigraphic correlations. Its common occurrence in the Latady Formation of the Orville Coast, Antarctica, indicates that at least part of this stratigraphic unit has a Kimmeridgian age. Although its precise taxonomic status remains in some doubt, it would appear to be the earliest buchiid-like bivalve so far recorded from the southern hemisphere. Its very wide distribution around the margins of Gondwana is similar to that established for species of the Late Jurassic bivalve genera Retroceramus, Buchia and Anopaea
The recovery of a 1.5 million yr long ice core from Antarctica represents a keystone of our understanding of Quaternary climate, the progression of glaciation over this time period and the role of greenhouse gas cycles in this progression. Here we tackle the question of where such ice may still be found in the Antarctic ice sheet. We can show that such old ice is most likely to exist in the plateau area of the East Antarctic ice sheet (EAIS) without stratigraphic disturbance and should be able to be recovered after careful pre-site selection studies. Based on a simple ice and heat flow model and glaciological observations, we conclude that positions in the vicinity of major domes and saddle position on the East Antarctic Plateau will most likely have such old ice in store and represent the best study areas for dedicated reconnaissance studies in the near future. In contrast to previous ice core drill site selections, however, we strongly suggest significantly reduced ice thickness to avoid bottom melting. For example for the geothermal heat flux and accumulation conditions at Dome C, an ice thickness lower than but close to about 2500 m would be required to find 1.5 Myr old ice (i.e., more than 700 m less than at the current EPICA Dome C drill site). Within this constraint, the resolution of an Oldest-Ice record and the distance of such old ice to the bedrock should be maximized to avoid ice flow disturbances, for example, by finding locations with minimum geothermal heat flux. As the geothermal heat flux is largely unknown for the EAIS, this parameter has to be carefully determined beforehand. In addition, detailed bedrock topography and ice flow history has to be reconstructed for candidates of an Oldest-Ice ice coring site. Finally, we argue strongly for rapid access drilling before any full, deep ice coring activity commences to bring datable samples to the surface and to allow an age check of the oldest ice.
Biological responses to climate and environmental changes in remote polar regions are of increasing interest in global change research. Terrestrial and marine polar ecosystems have suffered from impacts of both rapid climate change and intense human activities, and large fluctuations in the population sizes of seabirds, seals, and Antarctic krill have been observed in the past decades. To understand the mechanisms driving these regime shifts in polar ecosystems, it is important to first distinguish the influences of natural forcing from anthropogenic activities. Therefore, investigations of past changes of polar ecosystems prior to human contact are relevant for placing recent human-induced changes within a long-term historical context. Here we focus our review on the fossil, sub-fossil, archaeological, and biogeochemical remains of marine vertebrates in polar sediments. These remains include well-preserved tissues such as bones, hairs and feathers, and biogeochemical markers and other proxy indicators, including deposits of guano and excrement, which can accumulate in lake and terrestrial sediments over thousands of years. Analyses of these remains have provided insight into both natural and anthropogenic impacts on marine vertebrates over millennia and have helped identify the causal agents for these impacts. Furthermore, land-based seabirds and marine mammals have been shown to play an important role as bio-vectors in polar environments as they transport significant amounts of nutrients and anthropogenic contaminants between ocean and terrestrial ecosystems.
Modeling results have suggested that the circulation of the stratosphere and mesosphere in spring is strongly affected by the perturbations in heating induced by the Antarctic ozone hole. Here using both mesospheric MF radar wind observations from Rothera Antarctica (67°S, 68°W) as well as stratospheric analysis data, we present observational evidence that the stratospheric and mesospheric wind strengths are highly anti-correlated, and show their largest variability in November. We find that these changes are related to the total amount of ozone loss that occurs during the Antarctic spring ozone hole and particularly with the ozone gradients that develop between 57.5°S and 77.5°S. The results show that with increasing ozone loss during spring, winter conditions in the stratosphere and mesosphere persist longer into the summer. These results are discussed in the light of observations of the onset and duration of the Antarctic polar mesospheric cloud season
Over the last decade, two major calving events of the Petermann Ice Tongue in Northwest Greenland have led to speculation on its future stability and contribution to further Greenland Ice Sheet mass loss. However, it has been unclear if these events are anomalous or typical within the context of limited historical observations. We extend the historical record of the floating ice tongue using the stratigraphy of Petermann Fjord sediments to provide a longer-term perspective. Computed tomography (CT) scans, X-Ray Fluorescence (XRF) scans, Ice-Rafted Debris (IRD) counts, and the magnetic properties of specific particle size fractions constrain changes in depositional processes and sediment sources at our core sites, allowing for reconstructions of past behavior of the Petermann Ice Tongue. Radiocarbon dating of foraminifera, 210Pb, and paleomagnetic secular variation (PSV) provide age control and help to address uncertainties in radiocarbon reservoir ages. A floating ice tongue in Petermann Fjord formed in late glacial time as Petermann Glacier retreated from an advanced grounded position. This paleo-ice tongue broke-up during the early Holocene when high northern latitude summer insolation was higher than present. After gradual regrowth of the ice tongue associated with regional cooling, the ice tongue reached its historical extent only within the last millennium. Little or no ice tongue was present for nearly 5000 years during the middle Holocene, when decadal mean regional temperatures are estimated to be 0.8e2.9 °C higher than preindustrial (1750 CE) and seasonal sea-ice in the Lincoln Sea was reduced. This pre-historical behavior shows that recent anthropogenic warming may already be in the range of ice tongue instability and future projected warming increases the risk of ice tongue break-up by the mid- 21st Century.
A computationally predicted gene regulatory network (GRN), generated from mantle-specific gene expression profiles in the Antarctic clam Laternula elliptica, was interrogated to test the regulation and interaction of duplicated inducible hsp70 paralogues. hsp70A and hsp70B were identified in the GRN with each paralogue falling into unique submodules that were linked together by a single shared second neighbour. Annotations associated with the clusters in each submodule suggested that hsp70A primarily shares regulatory relationships with genes encoding ribosomal proteins, where it may have a role in protecting the ribosome under stress. hsp70B, on the other hand, interacted with a suite of genes involved in signalling pathways, including four transcription factors, cellular response to stress and the cytoskeleton. Given the contrasting submodules and associated annotations of the two hsp70 paralogues, the GRN analysis suggests that each gene is carrying out additional separate functions, as well as being involved in the traditional chaperone heat stress response, and therefore supports the hypothesis that subfunctionalization has occurred after gene duplication. The GRN was specifically produced from experiments investigating biomineralization; however, this study shows the utility of such data for investigating multiple questions concerning gene duplications, interactions and putative functions in a non-model species.
Studying the influence of changing environmental conditions on Antarctic marine benthic invertebrates is strongly constrained by limited access to the region, which poses difficulties to performing long-term experimental studies. Ecological modelling has been increasingly used as a potential alternative to assess the impact of such changes on species distribution or physiological performance.
The flow of carbon from atmosphere to sediment fauna and sediments reduces atmospheric CO2, which in turn reduces warming. Here, during the Changing Arctic Ocean Seafloor programme, we use comparable methods to those used in the Antarctic (vertical, calibrated camera drops and trawl-collected specimens) to calculate the standing stock of zoobenthic carbon throughout the Barents Sea. The highest numbers of morphotypes, functional groups and individuals were found in the northernmost sites (80–81.3° N, 29–30° E). Ordination (non-metric multidimensional scaling) suggested a cline of faunal transition from south to north. The functional group dominance differed across all six sites, despite all being apparently similar muds. Of the environmental variables we measured, only water current speed could significantly explain any of our spatial carbon differences. We found no obvious relationship with sea ice loss and thus no evidence of Arctic blue carbon–climate feedback. Blue carbon in the Barents Sea can be comparable with the highest levels in Antarctic shelf sediments. This article is part of the theme issue ‘The changing Arctic Ocean: consequences for biological communities, biogeochemical processes and ecosystem functioning’.
FacebookTwitterLinkedInEmailDigitalVision/Thinkstock(LANSING, Mich.) — A student who claims three Michigan State University basketball players gang-raped her three years ago is suing the institution in federal court for “discouraging” her from reporting the alleged assault.The civil lawsuit, which seeks both compensatory and punitive damages, was filed in the Michigan Southern District Court by the female plaintiff, referred to as Jane Doe. The suit names the university and the school’s staffers or counselors, who are referred to individually in the document as “Unidentified Roe” at the school’s counseling center.ABC News’ attempts to reach Michigan State University reps were not immediately returned.The document details what Doe claims happened the night of April 11, 2015, into the early morning hours of April 12, 2015.After the Michigan State University Spartans lost to the Duke Blue Devils, 81-61, some players appeared “sometime around midnight” at Harper’s Bar, where Doe was drinking with her roommate, according to the lawsuit.Jane Doe, then a freshman student majoring in sports journalism, said that three basketball team players eliminated from the tourney — referred to as John Doe 1, John Doe 2 and John Doe 3 — arrived and John Doe 1 approached her and “offered to buy her a drink,” according to the lawsuit.She accepted, the lawsuit states.Then the player introduced her to his two teammates, according to the lawsuit.According to the lawsuit, the woman had no romantic “interest in any of the team members” and merely believed she was commiserating with them based on her sports journalism career ambitions.The woman claims in the lawsuit that she was invited to attend a party at an off-campus apartment.Once at the party, the woman claims she was pulled into a bedroom and John Doe 1 allegedly told her: “You are mine for the night.”According to the lawsuit, the woman tried to play a particular song on a laptop when she noticed that “she could not manipulate her hands properly … [she] realized something was wrong and she thought she might have been drugged.”She was allegedly shown some basketball memorabilia by John Doe 2 and she requested some water “because she was incredibly thirsty,” according to the lawsuit.John Doe 2 brought her the water and took the freshman into his bedroom, where she assumed she would be shown more memorabilia.But while she took a sip of water, the room went dark, she claims in the lawsuit.Then, according to the lawsuit, the woman “was forcefully thrown face down on the bed, held in place so she could not move, while John Doe 2 raped [her] from behind.”The lawsuit goes on to allege the victim was crying as the act happened but was incapable of moving or speaking.“At no time did she consent to the sexual activity,” the lawsuit states.Then, after John Doe 2 was finished with the alleged rape, the document states that John Does 1 and 3 then entered the room, held her down, “and took turns raping her.”The woman claims that she awoke “a few hours later” on a couch inside John Doe 2’s apartment and called a taxi to take her back to her dorm room, where her roommate said that she had been looking for her all night “but could not find her,” the lawsuit states.The two students spoke about the alleged rape, according to the lawsuit, and the woman confided in a friend as well.Over a week passed until the friend escorted the alleged rape victim to Michigan State University Counseling Center to report the incident to a rape counselor, the lawsuit states.Upon disclosing that the three alleged attackers played on the school’s basketball squad the counselor “suddenly announced to Jane Doe that she needed another person in the room” and her “demeanor changed,” according to the lawsuit.A second member of the counseling center joined them, the lawsuit states, and the woman claims that she was given two options: to file a police report or “deal with the aftermath of the rape(s) on her own,” the lawsuit states.She was also allegedly informed by the two counselors that filing a police report would yield unwanted media attention, the lawsuit states. The woman also claims she was told “we have had many other students in the same situation who have reported, and it has been very traumatic for them,” according to the lawsuit.“If you pursue this, you are going to be swimming with some really big fish,” the woman alleges she was told, the lawsuit states.As a result, the alleged rape victim “became frightened to the point that she decided she could not report the rape(s) to law enforcement,” according to the lawsuit.Moreover, the lawsuit alleges that the university apparently failed to inform Jane Doe of her rights to file a no-contact order to ban any kind of contact with the ballplayers — whom she she said she occasionally came in contact with at her dorm.As a result, the woman didn’t report the incident for 10 months, the lawsuit states.By then, the woman become “so traumatized, depressed, and withdrawn” to the point that she was admitted to a psychiatric facility for treatment, according to the lawsuit.She quit school for a time and was refunded her tuition money, according to the lawsuit. She later returned, changing her major from sports journalism, a dream that had been “destroyed,” the lawsuit states.The lawsuit also claims that the school failed the woman by not informing her that she could report the incident to the Office of Institutional Equity nor did the school tell her about her Title IX rights — which grant her protections from sexual harassment.The lawsuit goes on to accuse the university of treating its male athletes “differently than they treated non-athlete related sexual assault complaints.”Beyond the damages the lawsuit is seeking, the alleged victim also wants Michigan State University to do away with an “unwritten, official” policy that the lawsuit characterizes as giving male athletes “unwritten permission to commit acts of sexual assault without consequence.The lawsuit also wants to establish a way to do away with the university’s “fostered culture in which female victims are discouraged from reported sexual assaults when those assaults are perpetrated by male athletes, thus protecting the university, the male athletics programs, and the male athletes at the expense of the female victims.”Copyright © 2018, ABC Radio. All rights reserved. April 10, 2018 /Sports News – National Michigan State University discouraged student from reporting alleged rape by athletes, lawsuit says Written by Beau Lund
Tags: Gunnison Football; Jamal Willis; Cutback Elite Speed Brad James Written by FacebookTwitterLinkedInEmailGUNNISON, Utah-Former BYU football star tailback Jamal Willis will be in Gunnison Saturday for a one-day speed-agility camp per the official Twitter account of Gunnison High School football.Willis, who played 11 games for the San Francisco 49ers in 1995, was a standout tailback at BYU from 1991-1994, amassing 4,065 scrimmage yards and 40 total touchdowns in his collegiate career.On his Twitter account, Willis promised participants that “cutback elite speed” is coming to Gunnison High School for his first traveling camp of the season.This camp will be at Gunnision High School on Saturday April 21 from 10:00 am-12:00 pm and costs $40.Participants can register by paying the $40 to Kera by Friday April 20.More information is available at goodtogreatathletics.com. April 17, 2018 /Sports News – Local Jamal Willis Coming To Gunnison High School For Football Clinic