MBNMS Draft Management Plan 6/2020
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1 Creating a Species Inventory for a Marine Protected Area: the Missing
Katherine R. Rice NOAA Species Inventory Project Spring 2018 Creating a Species Inventory for a Marine Protected Area: The Missing Piece for Effective Ecosystem-Based Marine Management Katherine R. Rice ABSTRACT Over the past decade, ecosystem-based management has been incorporated into many marine- management administrations as a marine-conservation tool, driven with the objective to predict, evaluate and possibly mitigate the impacts of a warming and acidifying ocean, and a coastline increasingly subject to anthropogenic control. The NOAA Office of National Marine Sanctuaries (ONMS) is one such administration, and was instituted “to serve as the trustee for a network of 13 underwater parks encompassing more than 600,000 square miles of marine and Great Lakes waters from Washington state to the Florida Keys, and from Lake Huron to American Samoa” (NOAA, 2015). The management regimes for nearly all national marine sanctuaries, as well as other marine protected areas, have the goal of managing and maintaining biodiversity within the sanctuary. Yet none of those sanctuaries have an inventory of their known species nor a standardized protocol for measuring or monitoring species biodiversity. Here, I outline the steps required to compile a species inventory for an MPA, but also describe some of stumbling blocks that one might encounter along the way and offer suggestions on how to handle these issues (see Appendix A: Process for Developing the MBNMS Species Inventory (PD-MBNMS)). This project consists of three research objectives: 1. Determining what species inventory efforts exist, how they operate, and their advantages and disadvantages 2. Determining the process of creating a species inventory 3. -
2019 Annual Report a SUMMARY Climate Change a Triple Threat for the Ocean CO2 Burning Fossil Fuels, Deforestation and Industrial Agriculture Release
2019 Annual Report A SUMMARY Climate Change A triple threat for the ocean CO2 Burning fossil fuels, deforestation and industrial agriculture release carbon dioxide (CO2) and other heat-trapping gases into our atmosphere, causing our planet to warm. The ocean has buffered us from the worst impacts of climate > 90% ~25% HEAT change by absorbing more than 90 CO2 percent of this excess heat and about 25 percent of the CO2, but at the cost of causing significant harm to marine ecosystems. LESS MORE WARMER OXYGEN ACIDIC SEA LEVEL BLEACHING TOXIC ALGAE HABITATS ACIDIFICATION FISHERIES Sea level rise is Warm-water coral reefs Larger and more frequent Lower oxygen levels More acidic water Disruptions in fisheries accelerating, flooding (marine biodiversity blooms are making fish, are suffocating some harms animals that build affect the marine food coastal communities hotspots) could be lost if birds, marine mammals marine animals and shells, such as corals, web, local livelihoods, and and drowning the planet warms by and people sick. shrinking their habitats. clams, and oysters. global food security. wetland habitats. 2°C (3.6°F). In 2019, the Intergovernmental Panel on Climate Change report details the triple threat of climate change to ocean ecosystems: Warming, acidification, and deoxygenation. annualreport.mbari.org/2019 Illustration by Emily Hess Cover photo: Animation by Frame 48 Source: IPCC, 2019: Special Report on the Ocean and Cryosphere in a Changing Climate (SROCC) View from the Masthead Climate Change A triple threat for the ocean CO 2 Advancing science Burning fossil fuels, deforestation and industrial agriculture release and engineering for carbon dioxide (CO2) and other heat-trapping gases into our atmosphere, causing our planet to Earth’s final frontier warm. -
Dam Effects on Low-Tide Channel Pools and Fish Use of Estuarine Habitat
Beaver in Tidal Marshes: Dam Effects on Low-Tide Channel Pools and Fish Use of Estuarine Habitat W. Gregory Hood Wetlands Official Scholarly Journal of the Society of Wetland Scientists ISSN 0277-5212 Wetlands DOI 10.1007/s13157-012-0294-8 1 23 Your article is protected by copyright and all rights are held exclusively by Society of Wetland Scientists. This e-offprint is for personal use only and shall not be self- archived in electronic repositories. If you wish to self-archive your work, please use the accepted author’s version for posting to your own website or your institution’s repository. You may further deposit the accepted author’s version on a funder’s repository at a funder’s request, provided it is not made publicly available until 12 months after publication. 1 23 Author's personal copy Wetlands DOI 10.1007/s13157-012-0294-8 ARTICLE Beaver in Tidal Marshes: Dam Effects on Low-Tide Channel Pools and Fish Use of Estuarine Habitat W. Gregory Hood Received: 31 August 2011 /Accepted: 16 February 2012 # Society of Wetland Scientists 2012 Abstract Beaver (Castor spp.) are considered a riverine or can have multi-decadal or longer effects on river channel form, lacustrine animal, but surveys of tidal channels in the Skagit riverine and floodplain wetlands, riparian vegetation, nutrient Delta (Washington, USA) found beaver dams and lodges in the spiraling, benthic community structure, and the abundance and tidal shrub zone at densities equal or greater than in non-tidal productivity of fish and wildlife (Jenkins and Busher 1979; rivers. Dams were typically flooded by a meter or more during Naiman et al. -
Spatial and Temporal Patterns of Salinity and Temperature at an Intertidal Groundwater Seep
Estuarine, Coastal and Shelf Science 72 (2007) 283e298 www.elsevier.com/locate/ecss Spatial and temporal patterns of salinity and temperature at an intertidal groundwater seep Ryan K. Dale*, Douglas C. Miller University of Delaware, College of Marine and Earth Studies, 700 Pilottown Road, Lewes, DE 19958, USA Received 9 June 2006; accepted 31 October 2006 Available online 22 December 2006 Abstract Spatial and temporal patterns at an intertidal groundwater seep at Cape Henlopen, Delaware, were characterized using a combination of pore water salinity and sediment temperature measurements. Pore water salinity maps, both on a small scale (resolution of 0.1 m over a 1.25 m2 area) and large scale (1e5 m over a 1710 m2 area) showed reduced pore water salinities to as low as one-sixth seawater strength in a region 0e6m from the intertidal beach slope break. In this region, there was substantial spatial variability in pore water salinity at all measured scales (0.1e 90 m) alongshore. At À10 cm sediment depth, pore water salinity ranged from 6 to 24 in less than 1 m horizontally. To further characterize spatial patterns in discharge, we used novel temperature probes during summer low tides and found temperatures were much lower in a ground- water seep than the nearby sediment, as much as 8e9 C cooler at À30 cm sediment depth. Measurements over time using temperature loggers showed that despite strong tidal and diel forcing on surficial sediment temperatures, thermal anomalies due to groundwater discharge persisted over several-day sampling periods and were strongest at À20 and À30 cm depth. -
Okeanos Explorer Rov Dive Summary
OKEANOS EXPLORER ROV DIVE SUMMARY Site Name GB907 Expedition Kelley Elliott/ Coordinator/ Brian Bingham ROV Lead Stephanie Farrington (Biology) Science Team Leads Jamie Austin (Geology) General Area Gulf of Mexico Descriptor Cruise Season Leg Dive Number ROV Dive Name EX1402 3 DIVE02 ROV: Deep Discoverer Equipment Deployed Camera Platform: Seirios CTD Depth Altitude Scanning Sonar USBL Position Heading ROV Measurements Pitch Roll HD Camera 1 HD Camera 2 Low Res Cam 1 Low Res Cam 2 Low Res Cam 3 Low Res Cam 4 Low Res Cam 2 Equipment N/A Malfunctions Dive Summary: EX1402L3_DIVE02 ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^ In Water at: 2014-04-13T13:45:38.439000 27°, 05.899' N ; 092°, 37.310' W Out Water at: 2014-04-13T19:12:34.841000 27°, 05.096' N ; 092°, 36.588' W ROV Dive Summary Off Bottom at: 2014-04-13T18:24:04.035000 (From processed ROV 27°, 05.455' N ; 092°, 36.956' W data) On Bottom at: 2014-04-13T14:31:16.507000 27°, 05.519' N ; 092°, 37.099' W Dive duration: 5:26:56 Bottom Time: 3:52:47 Max. depth: 1266.7 m Special Notes Primary Jamie Austin, EX, UT Austin, [email protected] Stephanie Farrington, EX, HBOI/FAU, [email protected] Andrea Quattrini, Temple, Temple, [email protected] Scientists Involved Bernie Ball, Duke, Duke, [email protected] (please provide name / Brian Kinlan, NOAA NMFS, [email protected] location / affiliation / email) Carolyn Ruppel, Woods Hole, USGS, [email protected] Erik Cordes, Temple, Temple, [email protected] Larry Mayer, UNH, UNH CCOM, [email protected] Michael Vecchione, -
Publications Supported by NOAA's Office of Ocean Exploration And
1 Publications Supported by NOAA’s Office of Ocean Exploration and Research Compiled by Chris Belter, NOAA Central Library Accurate as of 17 April 2012 Journal Articles (n=454) Ahyong ST. 2008. Deepwater crabs from seamounts and chemosynthetic habitats off eastern New Zealand (Crustacea : Decapoda : Brachyura). Zootaxa(1708):1-72. Aig D, Haywood K. 2008. Through the Sea Snow: The Central Role of Videography in the Deep Gulf Wrecks Mission. International Journal of Historical Archaeology 12(2):133-145. doi:10.1007/s10761-008-0049-7 Andrews AH, Stone RP, Lundstrom CC, DeVogelaere AP. 2009. Growth rate and age determination of bamboo corals from the northeastern Pacific Ocean using refined Pb-210 dating. Marine Ecology-Progress Series 397:173-185. doi:10.3354/meps08193 Angel MV. 2010. Towards a full inventory of planktonic Ostracoda (Crustacea) for the subtropical Northwestern Atlantic Ocean. Deep-Sea Research Part Ii-Topical Studies in Oceanography 57(24-26):2173-2188. doi:10.1016/j.dsr2.2010.09.020 Arellano SM, Young CM. 2009. Spawning, Development, and the Duration of Larval Life in a Deep-Sea Cold-Seep Mussel. Biological Bulletin 216(2):149-162. Auster PJ. 2007. Linking deep-water corals and fish populations. Bulletin of Marine Science 81:93-99. Auster PJ, Gjerde K, Heupel E, Watling L, Grehan A, Rogers AD. 2011. Definition and detection of vulnerable marine ecosystems on the high seas: problems with the "move-on" rule. ICES Journal of Marine Science 68(2):254-264. doi:10.1093/icesjms/fsq074 Auster PJ, Watling L. 2010. Beaked whale foraging areas inferred by gouges in the seafloor. -
A Guide to the Side of the Sea Lessons: Pre-Trip Activities Underwater Viewers Students Can Make Underwater Viewers for Studying Intertidal Life
Lessons The following lessons are grouped into three categories: pre-trip, during the trip, and post-trip. If you do pre-trip lessons, plan how to refer to them while on the trip. If you plan to do any of the post-trip lessons, be aware of ways to prepare the students while on the trip by making observations or asking questions. Each category is further divided into Hands-On Activities and Other Activities of various types. California State Content Standards that can easily be addressed through the lessons are referenced by subject and number. See pages 143–146 for abbreviated summaries of the standards. Some of the hands-on activities are intended to be discovery activities (experiments) in which the students don’t know the answers ahead of time. The teacher should try to facilitate the students’ discoveries rather than telling them what to expect. Whenever possible, be a guide on the side! Also . it is HIGHLY recommended that the teacher: • Try out all experiments before having students do them. • Enlist the help of parent volunteers before, during, and after experiments. • Feel free to adapt, expand, or alter experiments to suit your needs, student needs, and resources. Hands-on or “lab” type activities are presented in a detailed lesson plan format. A few “other” activities are given as examples, but the resources in the curriculum of the resources section (p. 158) give many additional worthwhile activities. Many of the lessons begin before the field trip and continue with activities to be done while at the coast. Others that are listed as pre-trip can also be done after the trip. -
Explore a Tide Pool Lesson Plan
Waldo County 4-H Program 992 Waterville Rd, Waldo, ME 04915 (207) 342-5971 Ext (800) 287-1426 toll free in Maine (800) 287-8957 TDD [email protected] [email protected] Putting knowledge to work with the people of Maine Explore a Tide Pool Purpose of activity: The purpose of this activity is to explore tide pools along the intertidal coastline. In this activity, youth will explore what a tide pool is and what type of plants and animals live there. What is a tide pool? Tide pools are rocky pools on the seashore that are filled with seawater when the ocean tide goes out, creating low tide. Tide pools often have plants and animals living in the pool that have to adapt to environmental extremes like the hot sun on a summer day and predators such as seagulls. Plants that grow in tide pools include seaweed, algae, and sea grass. Animals that live in tide pools might be periwinkles, crabs, starfish, barnacles, and more. Materials: An interactive On-line Tide Pool experience • Green Crab discovery with Tidepool Tim, of your choice. Gulf of Maine Inc • PBS Interactivities: Exploring Tide Pools • Intertidal snails with Tidepool Tim, Gulf • What is a Tide Pool? of Maine Inc • Tide Pool Ocean Adventure Children or • Tidal Pool Scavenger Hunt Handout Kids Activity • Ecosystem of California: Intertidal Instructions: 1. Take an adventure and explore tide pools. Choose one interactive on-line resource to view or take your family on an adventure to the nearest coastline and look for tidepools. If you and your family are preparing for a beach trip, make sure you bring appropriate beach clothes, shows with non-slip tread, and sun protection. -
Diversity of Intertidal Macroalgae Increases with Nitrogen Loading by Invertebrates
UC Davis UC Davis Previously Published Works Title Diversity of intertidal macroalgae increases with nitrogen loading by invertebrates Permalink https://escholarship.org/uc/item/47t5n0vn Journal Ecology, 85(10) ISSN 0012-9658 Authors Bracken, Matthew E S Nielsen, K J Publication Date 2004-10-01 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Ecology, 85(10), 2004, pp. 2828±2836 q 2004 by the Ecological Society of America DIVERSITY OF INTERTIDAL MACROALGAE INCREASES WITH NITROGEN LOADING BY INVERTEBRATES MATTHEW E. S. BRACKEN1,3 AND KARINA J. NIELSEN2 1Department of Zoology, Oregon State University, Corvallis, Oregon 97331-2914 USA 2Sonoma State University, Department of Biology, Rohnert Park, California 94928 USA Abstract. Many ecological phenomena are characterized by context dependency, and the relationship between diversity and productivity is no exception. We examined the re- lationship between macroalgal diversity and nutrient availability by evaluating the effects of reduced nutrients and their subsequent replacement via local-scale nutrient loading in tide pools. Macroalgae in Oregon coast high-intertidal pools have evolved in a nitrate-rich upwelling ecosystem, but instead of settling on low-intertidal reefs (where algae are often immersed in nutrient-rich nearshore waters) these individuals have colonized high-zone pools, where they are isolated from the ocean for extended periods of time and are subjected to extended periods of nitrate depletion. In some pools, this nutrient stress was ameliorated by a positive interaction: the excretion of ammonium by invertebrates. We conducted ex- perimental manipulations to quantify invertebrate-mediated ammonium loading and ma- croalgal ammonium uptake in high-intertidal pools. -
Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds
Appendix 5.4, Page 1 Appendix 5.4 Marine and Coastline Habitats Featured Species-associated Intertidal Habitats: Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds A swath of intertidal habitat occurs wherever the ocean meets the shore. At 44,000 miles, Alaska’s shoreline is more than double the shoreline for the entire Lower 48 states (ACMP 2005). This extensive shoreline creates an impressive abundance and diversity of habitats. Five physical factors predominantly control the distribution and abundance of biota in the intertidal zone: wave energy, bottom type (substrate), tidal exposure, temperature, and most important, salinity (Dethier and Schoch 2000; Ricketts and Calvin 1968). The distribution of many commercially important fishes and crustaceans with particular salinity regimes has led to the description of “salinity zones,” which can be used as a basis for mapping these resources (Bulger et al. 1993; Christensen et al. 1997). A new methodology called SCALE (Shoreline Classification and Landscape Extrapolation) has the ability to separate the roles of sediment type, salinity, wave action, and other factors controlling estuarine community distribution and abundance. This section of Alaska’s CWCS focuses on 3 main types of intertidal habitat: rocky intertidal, mudflats and beaches, and eelgrass beds. Tidal marshes, which are also intertidal habitats, are discussed in the Wetlands section, Appendix 5.3, of the CWCS. Rocky intertidal habitats can be categorized into 3 main types: (1) exposed, rocky shores composed of steeply dipping, vertical bedrock that experience high-to- moderate wave energy; (2) exposed, wave-cut platforms consisting of wave-cut or low-lying bedrock that experience high-to-moderate wave energy; and (3) sheltered, rocky shores composed of vertical rock walls, bedrock outcrops, wide rock platforms, and boulder-strewn ledges and usually found along sheltered bays or along the inside of bays and coves. -
National Oceanic and Atmospheric Administration
STATE OF CALIFORNIA—THE RESOURCES AGENCY ARNOLD SCHWARZENEGGER, GOVERNOR CALIFORNIA COASTAL COMMISSION 45 FREMONT, SUITE 2000 SAN FRANCISCO, CA 94105-2219 VOICE AND TDD (415) 904-5200 FAX (415) 904-5400 F4c STAFF REPORT AND RECOMMENDATION ON CONSISTENCY DETERMINATION Consistency Determination No. CD-011-07 Staff: CLT-SF File Date: 2/28/2007 60th Day: 4/29/2007 75th Day: 5/14/2007 Extended to: 8/17/2007 Commission Meeting: 8/10/2007 FEDERAL AGENCY: National Oceanic and Atmospheric Administration PROJECT LOCATION: The Monterey Bay National Marine Sanctuary extends from Marin County to Cambria (San Luis Obispo County), encompassing nearly 300 miles of shoreline and 5,322 square miles of ocean extending an average of twenty-five miles from shore (Exhibit 1). PROJECT DESCRIPTION: Revised management plan and revised set of regulations for the Monterey Bay National Marine Sanctuary. SUBSTANTIVE FILE DOCUMENTS: See page 37. CD-011-07 (NOAA) Monterey Bay National Marine Sanctuary Page 2 EXECUTIVE SUMMARY The National Oceanic and Atmospheric Administration (NOAA) submitted a consistency determination for the revised management plan and set of regulations governing activities in the Monterey Bay National Marine Sanctuary (MBNMS or Sanctuary). NOAA states that the proposed measures would afford better protection to the natural and cultural resources of the MBNMS. NOAA describes the proposed set of regulations as including both new regulations as well as changes to existing regulations, as follows: Proposed new regulations include prohibitions on: -
Burton 2013 Cultural History of Davidson Seamount
Cultural History of Davidson Seamount: A Characterization of Mapping, Research, and Fishing Erica J. Burton Monterey Bay National Marine Sanctuary Technical Report August 2013 Cultural History of Davidson Seamount MBNMS Technical Report COVER IMAGES Top left: Davidson Seamount, the first undersea feature to be officially termed a seamount by the U.S. Board on Geographic Names. This feature was surveyed by the C&GS in 1933 and named in honor of the great Coast Survey West Coast pioneer George Davidson, 1825-1911. Latitude should range from 35 to 36 degrees. Image Credit: NOAA Central Library Historical Collection (NOAA Photo Library) and original chart credit: Association of Commissioned Officers (1933). Top right: George Davidson (circa 1883). Credit: NOAA, B.A. Colonna Album (NOAA Photo Library) Bottom: Monterey Bay Aquarium Research Institute’s ROV Tiburon. Credit: T. Trejo for NOAA. SUGGESTED CITATION Burton, E.J. 2013. Cultural History of Davidson Seamount: A Characterization of Mapping, Research, and Fishing. MBNMS Technical Report, 21 p. 2 Cultural History of Davidson Seamount MBNMS Technical Report TABLE OF CONTENTS INTRODUCTION .......................................................................................................................................4 MAPPING ................................................................................................................................................................................ 5 RESEARCH AND MONITORING ................................................................................................................................