alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
## Breadcrumb

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#           Quantifying and addressing the prevalence and bias of study designs in the environmental and social sciences      

      December 11, 2020    

Building trust in science and evidence-based decision-making depends heavily on the credibility of studies and their findings. Researchers employ many different study designs that vary in their risk of bias to evaluate the true effect of interventions or impacts. Here, we empirically quantify, on a large scale, the prevalence of different study designs and the magnitude of bias in their estimates. Randomised designs and controlled observational designs with pre-intervention sampling were used by just 23% of intervention studies in biodiversity conservation, and 36% of intervention studies in social science. We demonstrate, through pairwise within-study comparisons across 49 environmental datasets, that these types of designs usually give less biased estimates than simpler observational designs. We propose a model-based approach to combine study estimates that may suffer from different levels of study design bias, discuss the implications for evidence synthesis, and how to facilitate the use of more credible study designs.

## Citation Information

## Related Content

                  -              Connect           

#### Barry P Baldigo

##### Research Biologist (RGE)

New York Water Science Center

bbaldigo@usgs.gov

518-285-5605

#### Deborah Buhl

##### Statistician

Northern Prairie Wildlife Research Center

dbuhl@usgs.gov

701-253-5532

#### Jill Shaffer

##### Ecologist

Northern Prairie Wildlife Research Center

jshaffer@usgs.gov

701-253-5547

####             Thomas Stanley, Ph.D. (Former Employee)          

##### Research Wildlife Biologist

Fort Collins Science Center

## Related Content

#### Barry P Baldigo

##### Research Biologist (RGE)

New York Water Science Center

bbaldigo@usgs.gov

518-285-5605

#### Deborah Buhl

##### Statistician

Northern Prairie Wildlife Research Center

dbuhl@usgs.gov

701-253-5532

#### Jill Shaffer

##### Ecologist

Northern Prairie Wildlife Research Center

jshaffer@usgs.gov

701-253-5547

####             Thomas Stanley, Ph.D. (Former Employee)          

##### Research Wildlife Biologist

Fort Collins Science Center

### Contact

####               Northern Prairie Wildlife Research Center          

8711 37th Street SoutheastJamestown, ND58401-7317United States

701-253-5500
Exhibit 32.1  CERTIFICATION OF CHIEF EXECUTIVE OFFICER

               PURSUANT TO 18 U.S.C. SS. 1350 ADOPTED PURSUANT TO
                  SECTION 906 OF THE SARBANES-OXLEY ACT OF 2002

         In connection with the quarterly Report of United EcoEnergy Corp.
(the "Company") on Form 10-Q for the period ended March 31, 2007 as
filed with the Securities and Exchange Commission on the date hereof (the
"Report"), I, William K. Mackey, Chief Executive Officer, certify pursuant
to 18 U.S.C. section 1350, as adopted pursuant to section 906 of the
Sarbanes-Oxley Act of 2002, that:

(1) The Report fully complies with the requirements of section 13(a) or 15(d)
of the Securities Exchange Act of 1934; and

(2) The information contained in the Report fairly presents, in all material
respects, the financial condition and result of operations of the Company.

/s/ William K. Mackey
---------------------------
William K. Mackey
Chief Executive Officer
May 14, 2007
Carlton D. HOLLIMAN, Appellant/Petitioner(s), v. STATE of Florida, Appellee/Respondent(s).

CASE NO.: 2D18-1882

District Court of Appeal of Florida, Second District.

June 25, 2018

**DECISION WITHOUT PUBLISHED OPINION**

Denied.
[Federal Register Volume 61, Number 161 (Monday, August 19, 1996)]
[Corrections]
[Page 42939]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: X96-40819]


-----------------------------------------------------------------------

INTERNATIONAL DEVELOPMENT COOPERATION AGENCY

Agency for International Development

48 CFR Parts 719, 722, and 752

[AIDAR Notice 96-1]
RIN 0412-AA29


Miscellaneous Amendments to Acquisition Regulations

Correction

    In rule document 96-18495 beginning on page 39089 in the issue of 
Friday, July 26, 1996, make the following corrections:


719.271-3  [Corrected]

    1. On page 39092, in the second column, the section heading, 
``718.271-3 [Amended]'' should read ``719.271-3 [Amended]''.


722.103-70  [Corrected]

    2. On the same page, in the same column, in amendatory instruction 
26 to section 722.103-70, in the third line, ``722.103.-1'' should read 
``722.103-1''.


722.805-70  [Corrected]

    3. On the same page, in the third column, in section 722.805-
70(b)(1)(i), in the second line, ``contract'' should read ``contact''.
    4. On the same page, in the same column, in section 722.805-
70(b)(1)(iii), in the last line, insert ``in'' after ``organizations''.


752.7028  [Corrected]

    5. On page 39096, in the second column, in amendatory instruction 
58 to section 752.7028, in the eighth line, ``sentence'' should read 
``sentences''.

BILLING CODE 1505-01-D
## Breadcrumb

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#           Tectonic activity as a significant source of crustal tetrafluoromethane emissions to the atmosphere: observations in groundwaters along the San Andreas Fault      

      February 1, 2015    

Tetrafluoromethane (CF4) concentrations were measured in 14 groundwater samples from the Cuyama Valley, Mil Potrero and Cuddy Valley aquifers along the Big Bend section of the San Andreas Fault System (SAFS) in California to assess whether tectonic activity in this region is a significant source of crustal CF4 to the atmosphere. Dissolved CF4 concentrations in all groundwater samples but one were elevated with respect to estimated recharge concentrations including entrainment of excess air during recharge (CreCre; ∼30 fmol kg−1 H2O), indicating subsurface addition of CF4 to these groundwaters. Groundwaters in the Cuyama Valley contain small CF4 excesses (0.1–9 times CreCre), which may be attributed to an in situ release from weathering and a minor addition of deep crustal CF4 introduced to the shallow groundwater through nearby faults. CF4 excesses in groundwaters within 200 m of the SAFS are larger (10–980 times CreCre) and indicate the presence of a deep crustal flux of CF4 that is likely associated with the physical alteration of silicate minerals in the shear zone of the SAFS. Extrapolating CF4 flux rates observed in this study to the full extent of the SAFS (1300 km × 20–100 km) suggests that the SAFS potentially emits (0.3–1)×10−1 kg(0.3–1)×10−1 kg CF4 yr−1 to the Earth's surface. For comparison, the chemical weathering of ∼7.5×104 km2∼7.5×104 km2 of granitic rock in California is estimated to release (0.019–3.2)×10−1 kg(0.019–3.2)×10−1 kg CF4 yr−1. Tectonic activity is likely an important, and potentially the dominant, driver of natural emissions of CF4 to the atmosphere. Variations in preindustrial atmospheric CF4 as observed in paleo-archives such as ice cores may therefore represent changes in both continental weathering and tectonic activity, including changes driven by variations in continental ice cover during glacial–interglacial transitions.

## Citation Information

## Related Content

                  -              Connect           

#### Justin Kulongoski

##### Research Hydrologist

California Water Science Center

kulongos@usgs.gov

619-225-6122

#### Daniel Deeds

##### Chief, Bridgeville Hydrologic Studies

Pennsylvania Water Science Center

ddeeds@usgs.gov

## Related Content

#### Justin Kulongoski

##### Research Hydrologist

California Water Science Center

kulongos@usgs.gov

619-225-6122

#### Daniel Deeds

##### Chief, Bridgeville Hydrologic Studies

Pennsylvania Water Science Center

ddeeds@usgs.gov

### Study Area

### Contact

####               Sacramento Projects Office (USGS California Water Science Center)          

6000 J Street, Placer HallSacramento, CA95819United States

916-278-3000

916-278-3070

### Explore Search

                  - Water
                  - United States
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                  -  Mil Potrero and Cuddy Valley
                  - california

View All **
# C_2005053EN.01001501.xml

| 3.3.2005 | EN | Official Journal of the European Union | C 53/15 |
| --- | --- | --- | --- |

3.3.2005

EN

Official Journal of the European Union

C 53/15

---

COUNCIL DECISION

COUNCIL DECISION

of 17 February 2005

renewing the term of office of the President of the Office for Harmonisation in the Internal Market (trade marks and designs)

(2005/C 53/02)

THE COUNCIL OF THE EUROPEAN UNION,

Having regard to the Treaty establishing the European Community,

Having regard to Council Regulation (EC) No 40/94 of 20 December 1993 on the Community trade mark (1), and in particular Article 120(1) and (2) thereof,

1

Having regard to the Council Decision of 2 May 2000 appointing the President of the Office for Harmonisation in the Internal Market (trade marks and designs) (2),

2

Having regard to the proposal by the Administrative Board of the Office for Harmonisation in the Internal Market (trade marks and designs) of 23 November 2004 concerning the renewal of the term of office of the President of the Office,

HAS DECIDED AS FOLLOWS:

Sole Article

The term of office of Mr Wubbo de BOER, born on 27 May 1948, as President of the Office for Harmonisation in the Internal Market (trade marks and designs) is hereby renewed for the period from 1 October 2005 to 30 September 2010.

Done at Brussels, 17 February 2005.

For the Council

The President

J.-C. JUNCKER

---

(1)  OJ L 11, 14.1.1994, p. 1. Regulation as last amended by Regulation (EC) No 422/2004 (OJ L 70, 9.3.2004, p. 1).

1

(2)  OJ C 139, 18.5.2000, p. 1.

2

---
Exhibit 31.2

                                 Certifications

I, Ludovic Payage, certify that:

     1. I have reviewed this annual report on Form 10-KSB of Poseidis, Inc.

     2. Based on my  knowledge,  this annual  report does not contain any untrue
statement of a material fact or omit to state a material fact  necessary to make
the statements made, in light of the  circumstances  under which such statements
were made,  not  misleading  with  respect to the period  covered by this annual
report.

     3. Based on my knowledge,  the financial  statements,  and other  financial
information  included  in this annual  report,  fairly  present in all  material
respects the financial  condition,  results of operations  and cash flows of the
registrant as of, and for, the periods presented in this annual report.

     4. The  registrant's  other  certifying  officers and I are responsible for
establishing and maintaining  disclosure  controls and procedures (as defined in
exchange act rules 13a-14 and 15d-14) for the registrant and have:

     A)   designed  such  disclosure  controls  and  procedures  to ensure  that
          material  information  relating  to  the  registrant,   including  its
          consolidated subsidiaries,  is made known to us by others within those
          entities,  particularly  during the period in which this annual report
          is being prepared;
     B)   evaluated the  effectiveness of the registrant's  disclosure  controls
          and procedures as of a date within 90 days prior to the filing date of
          this annual report (the "evaluation date"); and
     C)   presented   in  this   annual   report  our   conclusions   about  the
          effectiveness  of the disclosure  controls and procedures based on our
          evaluation as of the evaluation date;

     5. The registrant's other certifying  officers and I have disclosed,  based
on our most  recent  evaluation,  to the  registrant's  auditors  and the  audit
committee  of  registrant's  board  of  directors  (or  persons  performing  the
equivalent functions):

     A)   all  significant  deficiencies  in the design or operation of internal
          controls  which could  adversely  affect the  registrant's  ability to
          record,  process,   summarize  and  report  financial  data  and  have
          identified for the  registrant's  auditors any material  weaknesses in
          internal controls; and
     B)   any fraud, whether or not material,  that involves management or other
          employees who have a  significant  role in the  registrant's  internal
          controls.

Date: June 10, 2004

/s/ Ludovic Payage
Ludovic Payage
Chief Financial Officer (or equivalent)
## Breadcrumb

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#           South Dakota and Landsat      

      June 16, 2021    

View Report

Version History

XML Format

HTML Format

Few States derive as much of their social and economic well-being from the land as South Dakota. Agriculture is the State’s primary industry. Hunting, fishing, tourism, mining, and hydroelectric power are also important economic and cultural drivers. Data from the U.S. Geological Survey Landsat program, archived at the U.S. Geological Survey Earth Resources Observation and Science Center just outside Sioux Falls, South Dakota, has long been a boon to the monitoring, mapping, and management of the State’s land resources.

## Citation Information

### Study Area

### Contact

####               Earth Resources Observation and Science (EROS) Center          

47914 252nd StreetSioux Falls, SD57198United States

custserv@usgs.gov

800-252-4547

### Explore Search

                  - Information Systems
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                  - South Dakota

View All **
**EXHIBIT31.2****CERTIFICATIONS**I, Yucheng Ding, Co- Chief Executive Officer of Sun New Media, Inc., certify that 1. I have reviewed this annual report on Form 10-KSB of Sun New Media, Inc.; 2. Based on my knowledge, this report does not contain any untrue statement of a material factor omit to state a material fact necessary to make the statements made, in light of thecircumstances under which such statements were made, not misleading with respect to the periodcovered by this report; 3. Based on my knowledge, the financial statements, and other financial information included inthis report, fairly present in all material respects the financial condition, results ofoperations and cash flows of the registrant as of, and for, the periods presented in thisreport; 4. The registrant’s other certifying officers and I are responsible for establishing andmaintaining disclosure controls and procedures (as defined in Exchange Act Rules 13a-15 (e)and 15d-15 (e)) for the registrant and we have: (a) designed such disclosure controls and procedures, or caused suchdisclosure controls and procedures to be designed under our supervision,to ensure that material information relating to the registrant, includingits consolidated subsidiaries, is made known to us by others within thoseentities, particularly during the period in which this report was beingprepared; (b) evaluated the effectiveness of the registrant’s disclosure controls andprocedures and presented in this report our conclusions about theeffectiveness of the disclosure controls and procedures, as of the end ofthe period covered by this report based on such evaluation; and (c) disclosed in this report any change in the registrant’s internal controlover financial reporting that occurred during the registrant’s mostrecent fiscal quarter (the registrant’s fourth fiscal quarter in the caseof an annual report) that has materially affected, or is reasonablylikely to materially affect, the registrant’s internal control overfinancial reporting; and5. The registrant’s other certifying officers and I have disclosed, based on our most recentevaluation of internal control over financial reporting, to the registrant’s auditors and theaudit committee of registrant’s board of directors (or persons performing the equivalentfunction): (a) all significant deficiencies and material weaknesses in the design oroperation of internal control over financial reporting which arereasonably likely to adversely affect the registrant’s ability to record,process, summarize and report financial information; and (b) any fraud, whether or not material, that involves management or otheremployees who have a significant role in the registrant’s internalcontrol over financial reporting./s/ Yucheng Ding Yucheng Ding, Co-Chief Executive Officer and DirectorDate: January 13, 2006
## Breadcrumb

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#           Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1980      

      January 1, 1980    

View Document

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.

## Citation Information

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                  - Natural Hazards
                  - United States
                  - Alaska
                  - College Observatory

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#           Klamath Falls earthquakes, September 20, 1993 — Including the strongest quake ever measured in Oregon      

      November 1, 1993    

Earthquakes struck the Klamath Falls area on Monday night, September 20, 1993, resulting in two deaths and extensive damage. The quakes were felt as far away as Coos Bay to the west, Eugene to the north, Lakeview to the east, and Chico, California, to the south. 

A foreshock recorded at 8:16 p.m. had a Richter magnitude of 3.9. The first of two main shocks, measuring 5.9 on the Richter scale, rumbled through Klamath Falls at 8:28 p.m. Following 16 smaller jolts with magnitudes between 2.2 and 3.8, the largest quake struck at 10:45 p.m. This earthquake, measuring 6.0 on the Richter scale, is the largest to hit Oregon since the 1873 Port Orford/Crescent City earthquake (Jacobson, 1986). Oregon has been shaken by stronger quakes, but those quakes originated beneath the Pacific Ocean west of Port Orford. 

## Citation Information

## Related Content

                  -              Connect           

#### Ray Wells

##### Research Geologist

Geology, Minerals, Energy, and Geophysics Science Center

rwells@usgs.gov

## Related Content

#### Ray Wells

##### Research Geologist

Geology, Minerals, Energy, and Geophysics Science Center

rwells@usgs.gov

### Study Area

### Contact

#### Geologic Hazards Science Center

1711 Illinois St.Golden, CO80401United States

303-273-8500

####               Geology, Minerals, Energy, and Geophysics Science Center          

Building 19, 350 N. Akron Rd.P.O. Box 158Moffett Field, CA94035United States

#### USGS Volcano Science Center

1300 SE Cardinal CourtVancouver, WA38683United States

360-993-8900

### Explore Search

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DOCSBHM\2317202\1

UNITED STATES BANKRUPTCY COURT

FOR THE SOUTHERN DISTRICT OF FLORIDA (Miami)

In re: Case No. 20-14695-LMI

Cinemex USA Real Estate Holdings, Inc., Chapter 11

Debtor(s).

______________________________________________________________________________

NOTICE OF APPEARANCE

Stephen B. Porterfield of the law firm of Sirote & Permutt, P.C. hereby notifies the Court 

and all interested parties of his representation of Cobb Lakeside, LLC and Cobb Theaters III, 

LLC in this case and respectfully requests electronic notification of all filings and other notices 

entered in this case at the following email address: sporterfield@sirote.com.

/s/ Stephen B. Porterfield

Stephen B. Porterfield

Counsel for Cobb Lakeside, LLC and Cobb 

Theaters III, LLC

OF COUNSEL:

SIROTE & PERMUTT, P.C.

2311 Highland Avenue South

P.O. Box 55727

Birmingham, AL 35255-5727

Tel.: (205) 930-5278

Fax: (205) 212-3862

sporterfield@sirote.com

Case 20-14695-LMI Doc 61 Filed 05/06/20 Page 1 of 2
DOCSBHM\2317202\1

CERTIFICATE OF SERVICE

I hereby certify that on May 6, 2020, I electronically filed the foregoing with the Clerk of 

Court via the CM/ECF filing system which will provide notice to all interested parties, including 

the following:

Brett M. Amron, Esq.

Jeffrey P. Bast, Esq.

Jaime Burton Leggett

1 SE 3 Avenue #1400

Miami, FL 33131

bamron@bastamron.com

jabast@bastamron.com

jleggett@bastamron.com

Patricia B. Tomasco

700 Louisiana, Suite 500

Houston, TX 77002

pattytomasco@quinnemanuel.com

U.S. Trustee

Office of the U.S. Trustee

51 S.W. 1st Avenue

Suite 1204

Miami, FL 33130

/s/ Stephen B. Porterfield

OF COUNSEL

Case 20-14695-LMI Doc 61 Filed 05/06/20 Page 2 of 2
## Breadcrumb

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#           Revised ages for tuffs of the Yellowstone Plateau volcanic field: Assignment of the Huckleberry Ridge Tuff to a new geomagnetic polarity event      

      January 1, 2002    

40Ar/39Ar ages were determined on the three major ash-flow tuffs of the Yellowstone Plateau volcanic field in the region of Yellowstone National Park in order to improve the precision of previously determined ages. Total-fusion and incremental- heating ages of sanidine yielded the following mean ages: Huckleberry Ridge Tuff—2.059 ± 0.004 Ma; Mesa Falls Tuff— 1.285 ± 0.004 Ma; and Lava Creek Tuff— 0.639 ± 0.002 Ma. The Huckleberry Ridge Tuff has a transitional magnetic direction and has previously been related to the Reunion Normal- Polarity Subchron. Dating of the Reunion event has been reviewed and its ages have been normalized to a common value for mineral standards. The age of the Huckleberry Ridge Tuff is significantly younger than lava flows of the Reunion event on Ré union Island, supporting other evidence for a normal-polarity event younger than the Reunion event.

## Citation Information

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### Contact

#### USGS Volcano Science Center

1300 SE Cardinal CourtVancouver, WA38683United States

360-993-8900

### Explore Search

                  - Natural Hazards
                  - United States
                  - Yellowstone National Park
                  - Idaho
                  -  Montana
                  -  Wyoming

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